From c38a7232e842f38bc73f4af00c7d5412290e90cc Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Tue, 12 Dec 2023 12:12:01 +0100
Subject: [PATCH 01/38] Initial plugins

---
 .../CMakeLists.txt                            |  44 ++
 .../lithosphere_rift_IC.cc                    | 396 ++++++++++++++++++
 .../lithosphere_rift_IC.h                     | 147 +++++++
 .../lithosphere_rift_IT.h                     | 152 +++++++
 .../lithosphere_rift_IT_2.cc                  | 320 ++++++++++++++
 .../rift_box_initial_plastic_strain.cc        | 341 +++++++++++++++
 .../rift_box_initial_plastic_strain.h         | 162 +++++++
 7 files changed, 1562 insertions(+)
 create mode 100644 cookbooks/initial_conditions_continental_rift/CMakeLists.txt
 create mode 100644 cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
 create mode 100644 cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
 create mode 100644 cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
 create mode 100644 cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
 create mode 100644 cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
 create mode 100644 cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h

diff --git a/cookbooks/initial_conditions_continental_rift/CMakeLists.txt b/cookbooks/initial_conditions_continental_rift/CMakeLists.txt
new file mode 100644
index 00000000000..5763297edab
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/CMakeLists.txt
@@ -0,0 +1,44 @@
+# Copyright (C) 2015 - 2021 by the authors of the ASPECT code.
+#
+# This file is part of ASPECT.
+#
+# ASPECT is free software; you can redistribute it and/or modify
+# it under the terms of the GNU General Public License as published by
+# the Free Software Foundation; either version 2, or (at your option)
+# any later version.
+#
+# ASPECT is distributed in the hope that it will be useful,
+# but WITHOUT ANY WARRANTY; without even the implied warranty of
+# MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE.  See the
+# GNU General Public License for more details.
+#
+# You should have received a copy of the GNU General Public License
+# along with ASPECT; see the file LICENSE.  If not see
+# <http://www.gnu.org/licenses/>.
+
+CMAKE_MINIMUM_REQUIRED(VERSION 3.1.0)
+
+FIND_PACKAGE(Aspect 2.4.0 QUIET HINTS ${Aspect_DIR} ../ ../../ $ENV{ASPECT_DIR})
+
+IF (NOT Aspect_FOUND)
+  MESSAGE(FATAL_ERROR "\n"
+    "Could not find a valid ASPECT build/installation directory. "
+    "Please specify the directory where you are building ASPECT by passing\n"
+    "   -D Aspect_DIR=<path to ASPECT>\n"
+    "to cmake or by setting the environment variable ASPECT_DIR in your shell "
+    "before calling cmake. See the section 'How to write a plugin' in the "
+    "manual for more information.")
+ENDIF ()
+
+DEAL_II_INITIALIZE_CACHED_VARIABLES()
+
+SET(TARGET "initial_conditions_continental_rift")
+PROJECT(${TARGET})
+
+ADD_LIBRARY(${TARGET} SHARED 
+lithosphere_rift_IC.cc
+lithosphere_rift_IT_2.cc
+lithosphere_rift_topo.cc
+rift_box_initial_plastic_strain.cc
+)
+ASPECT_SETUP_PLUGIN(${TARGET})
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
new file mode 100644
index 00000000000..808a4349b49
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
@@ -0,0 +1,396 @@
+/*
+  Copyright (C) 2017 by the authors of the ASPECT code.
+
+  This file is part of ASPECT.
+
+  ASPECT is free software; you can redistribute it and/or modify
+  it under the terms of the GNU General Public License as published by
+  the Free Software Foundation; either version 2, or (at your option)
+  any later version.
+
+  ASPECT is distributed in the hope that it will be useful,
+  but WITHOUT ANY WARRANTY; without even the implied warranty of
+  MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE.  See the
+  GNU General Public License for more details.
+
+  You should have received a copy of the GNU General Public License
+  along with ASPECT; see the file LICENSE.  If not see
+  <http://www.gnu.org/licenses/>.
+*/
+
+
+#include "lithosphere_rift_IC.h"
+#include "lithosphere_rift_IT.h"
+#include <aspect/geometry_model/box.h>
+#include <aspect/utilities.h>
+
+
+namespace aspect
+{
+  namespace InitialComposition
+  {
+    template <int dim>
+    void
+    LithosphereRift<dim>::
+    initialize ()
+    {
+      // Check that the required initial composition model is used
+      const std::vector<std::string> active_initial_temperature_models = this->get_initial_temperature_manager().get_active_initial_temperature_names();
+      AssertThrow(find(active_initial_temperature_models.begin(),active_initial_temperature_models.end(), "lithosphere with rift") != active_initial_temperature_models.end(),
+                  ExcMessage("The lithosphere with rift initial composition plugin requires the lithosphere with rift initial temperature plugin."));
+    }
+
+    template <int dim>
+    double
+    LithosphereRift<dim>::
+    initial_composition (const Point<dim> &position,
+                         const unsigned int compositional_index) const
+    {
+      // Retrieve the indices of the fields that represent the lithospheric layers.
+      // We assume a 3-layer system with an upper crust, lower crust and lithospheric mantle
+      const unsigned int id_upper = this->introspection().compositional_index_for_name("upper");
+      const unsigned int id_lower = this->introspection().compositional_index_for_name("lower");
+      const unsigned int id_mantle_L = this->introspection().compositional_index_for_name("mantle_L");
+
+      // Determine coordinate system
+      const bool cartesian_geometry = dynamic_cast<const GeometryModel::Box<dim> *>(&this->get_geometry_model()) != NULL ? true : false;
+
+      const Point<dim-1> surface_point = surface_position(position, cartesian_geometry);
+
+      // Get the distance to the line segments along a path parallel to the surface
+      const double distance_to_rift_axis = distance_to_rift(surface_point);
+
+      // Get the signed distance to a polygon of different lithospheric thicknesses
+      const std::pair<double, unsigned int> distance_to_L_polygon = distance_to_polygon(surface_point);
+
+      // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
+      // (in this exact order) based on the distance from the rift axis.
+      const double local_upper_crust_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][0]
+                                                  +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[0])
+                                                 * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      const double local_lower_crust_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
+                                                  +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
+                                                 * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      const double local_mantle_lithosphere_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
+                                                         +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
+                                                        *  (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+
+//sb      std::cout << "Initial compo " << position[0] << " " << compositional_index << " " << local_upper_crust_thickness << " " << local_lower_crust_thickness << " " << local_mantle_lithosphere_thickness << std::endl;
+
+      // Compute depth
+      const double depth = this->get_geometry_model().depth(position);
+
+      // Check which layer we're in and return value.
+      if (depth <= local_upper_crust_thickness && compositional_index == id_upper)
+        return 1.;
+      else if (depth > local_upper_crust_thickness && depth <= local_upper_crust_thickness+local_lower_crust_thickness && compositional_index == id_lower)
+        return 1.;
+      else if (depth > local_upper_crust_thickness+local_lower_crust_thickness && depth <= local_upper_crust_thickness+local_lower_crust_thickness+local_mantle_lithosphere_thickness && compositional_index == id_mantle_L)
+        return 1.;
+      else
+        return 0.;
+    }
+
+    template <int dim>
+    double
+    LithosphereRift<dim>::
+    distance_to_rift (const Point<dim-1> &surface_position) const
+    {
+      // Initiate distance with large value
+      double distance_to_rift_axis = 1e23;
+      double temp_distance = 0;
+
+      // Loop over all line segments
+      for (unsigned int i_segments = 0; i_segments < point_list.size(); ++i_segments)
+        {
+          temp_distance = (dim == 2) ? std::abs(surface_position[0]-point_list[i_segments][0][0]) : std::abs(Utilities::distance_to_line(point_list[i_segments], Point<2>(surface_position[0],surface_position[dim-2])));
+
+          // Get the minimum distance
+          distance_to_rift_axis = std::min(distance_to_rift_axis, temp_distance);
+        }
+
+      return distance_to_rift_axis;
+    }
+
+    template <int dim>
+    Point<dim-1>
+    LithosphereRift<dim>::
+    surface_position (const Point<dim> &position,
+                      const bool cartesian_geometry) const
+    {
+      Point<dim-1> surface_point;
+      if (cartesian_geometry)
+        {
+          for (unsigned int d=0; d<dim-1; ++d)
+            surface_point[d]=position[d];
+        }
+      // chunk (spherical) geometries
+      else
+        {
+          // spherical coordinates in radius [m], lon [rad], colat [rad] format
+          const std::array<double,dim> spherical_point = Utilities::Coordinates::cartesian_to_spherical_coordinates(position);
+          // return lon [degrees], lat [degrees]
+          for (unsigned int d=0; d<dim-1; ++d)
+            surface_point[d] = spherical_point[d+1]*180./numbers::PI;
+          if (dim == 3)
+            surface_point[dim-2] = 90. - surface_point[dim-2];
+        }
+
+      return surface_point;
+    }
+
+    template <int dim>
+    std::pair<double,unsigned int>
+    LithosphereRift<dim>::
+    distance_to_polygon (const Point<dim-1> &surface_position) const
+    {
+      // Inside is positive, outside negative. We assume no overlap of the different polygons.
+      double max_distance = -1e24;
+      unsigned int max_distance_polygon = 0;
+      for (unsigned int n = 0; n<polygon_point_list.size(); ++n)
+        {
+          double temp_distance = 0;
+          if (dim == 2)
+            {
+              double sign = -1.;
+              if (surface_position[0]>polygon_point_list[n][0][0] && surface_position[0]<polygon_point_list[n][1][0])
+                sign = 1.;
+              temp_distance = sign * std::min(std::abs(polygon_point_list[n][1][0] - surface_position[0]), std::abs(surface_position[0] - polygon_point_list[n][0][0]));
+            }
+          else
+            {
+              temp_distance = Utilities::signed_distance_to_polygon<dim>(polygon_point_list[n], Point<2>(surface_position[0],surface_position[dim-2]));
+//sb             std::cout << "Distance to polygon " << n << " " << surface_position << " " << temp_distance << std::endl;
+            }
+
+//          std::cout << "Distance to polygon " << dim << " " << surface_position << " " << temp_distance << std::endl;
+          if (temp_distance > max_distance)
+            {
+              max_distance = temp_distance;
+              max_distance_polygon = n;
+            }
+        }
+      return std::pair<double, unsigned int> (max_distance, max_distance_polygon);
+    }
+
+    template <int dim>
+    void
+    LithosphereRift<dim>::declare_parameters (ParameterHandler &prm)
+    {
+      prm.enter_subsection ("Initial composition model");
+      {
+        prm.enter_subsection("Lithosphere with rift");
+        {
+          prm.declare_entry ("Standard deviation of Gaussian rift geometry", "20000",
+                             Patterns::Double (0),
+                             "The standard deviation of the Gaussian distribution of the amplitude of the strain noise. "
+                             "Note that this parameter is taken to be the same for all rift segments. "
+                             "Units: $m$ or degrees.");
+          prm.declare_entry ("Half width of polygon smoothing", "20000",
+                             Patterns::Double (0),
+                             "The half width of the hyperbolic tangent smoothing used to transition to the lithospheric thicknesses of the polygon. "
+                             "Note that this parameter is taken to be the same for all polygons. "
+                             "Units: $m$ or degrees.");
+          prm.declare_entry ("Blend polygons and rifts", "true",
+                             Patterns::Bool (),
+                             "Whether or not to blend the contributions of polygons and the rift. For true, they're blend together. "
+                             "For false, the polygon thicknesses are taken as the local thicknesses. "
+                             "Units: /.");
+          prm.declare_entry ("Amplitude of Gaussian rift geometry", "0.2",
+                             Patterns::List(Patterns::Double (-1,1)),
+                             "The amplitude of the Gaussian distribution of the amplitude of the strain noise. "
+                             "Note that this parameter is taken to be the same for all rift segments, but can "
+                             "vary per lithosphere layer. "
+                             "Units: none.");
+          prm.declare_entry ("Layer thicknesses", "30000.",
+                             Patterns::List(Patterns::Double(0)),
+                             "List of thicknesses for the bottom of the lithospheric layers,"
+                             "for a total of N+1 values, where N is the number of compositional fields."
+                             "If only one value is given, then all use the same value.  Units: $m$");
+          prm.declare_entry ("Rift axis line segments",
+                             "",
+                             Patterns::Anything(),
+                             "Set the line segments that represent the rift axis. Each segment is made up of "
+                             "two points that represent horizontal coordinates (x,y) or (lon,lat). "
+                             "The exact format for the point list describing the segments is "
+                             "\"x1,y1>x2,y2;x2,y2>x3,y3;x4,y4>x5,y5\". Note that the segments can be connected "
+                             "or isolated. The units of the coordinates are "
+                             "dependent on the geometry model. In the box model they are in meters, in the "
+                             "chunks they are in degrees.");
+          prm.declare_entry ("Lithospheric polygons",
+                             "",
+                             Patterns::List(Patterns::Anything()),
+                             "Set the polygons that represent an area of different lithospheric thickness. "
+                             "The polygons are separated by semicolons."
+                             "Each polygon is a list of "
+                             "points that represent horizontal coordinates (x,y) or (lon,lat). "
+                             "The exact format for the point list describing a polygon is "
+                             "\"x1,y1>x2,y2>x3,y3>x4,y4>x5,y5\". Note that the polygon is assumed to be closed. "
+                             "The units of the coordinates are "
+                             "dependent on the geometry model. In the box model they are in meters, in the "
+                             "chunks they are in degrees.");
+          prm.declare_entry ("Lithospheric polygon layer thicknesses", "30000.",
+                             Patterns::List(Patterns::List(Patterns::Double(0),0,3,","),0,10,";"),
+                             "List of thicknesses of the lithospheric layers for each polygon."
+                             "For each polygon a total of 3 values should be given (upper crust, lower crust, mantle lithosphere)."
+                             "If only one value is given, then all use the same value.  Units: $m$");
+
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+    }
+
+    template <int dim>
+    void
+    LithosphereRift<dim>::parse_parameters (ParameterHandler &prm)
+    {
+      // Check that the required compositional fields exist.
+      AssertThrow(this->introspection().compositional_name_exists("upper"),ExcMessage("We need a compositional field called 'upper' representing the upper crust."));
+      AssertThrow(this->introspection().compositional_name_exists("lower"),ExcMessage("We need a compositional field called 'lower' representing the lower crust."));
+      AssertThrow(this->introspection().compositional_name_exists("mantle_L"),ExcMessage("We need a compositional field called 'mantle_L' representing the lithospheric part of the mantle."));
+
+      prm.enter_subsection ("Initial composition model");
+      {
+        prm.enter_subsection("Lithosphere with rift");
+        {
+          sigma_rift             = prm.get_double ("Standard deviation of Gaussian rift geometry");
+          sigma_polygon          = prm.get_double ("Half width of polygon smoothing");
+          blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
+          A                      = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
+                                                                           3,
+                                                                           "Amplitude of Gaussian rift geometry");
+          thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
+                                                                3,
+                                                                "Layer thicknesses");
+          // Read in the string of segments
+          const std::string temp_all_segments = prm.get("Rift axis line segments");
+          // Split the string into segment strings
+          const std::vector<std::string> temp_segments = Utilities::split_string_list(temp_all_segments,';');
+          const unsigned int n_temp_segments = temp_segments.size();
+          point_list.resize(n_temp_segments);
+          // Loop over the segments to extract the points
+          for (unsigned int i_segment = 0; i_segment < n_temp_segments; i_segment++)
+            {
+              // In 3d a line segment consists of 2 points,
+              // in 2d only 1 (ridge axis orthogonal to x and y)
+
+              const std::vector<std::string> temp_segment = Utilities::split_string_list(temp_segments[i_segment],'>');
+
+              if (dim == 3)
+                {
+                  AssertThrow(temp_segment.size() == 2,ExcMessage ("The given coordinate '" + temp_segment[i_segment] + "' is not correct. "
+                                                                   "It should only contain 2 parts: "
+                                                                   "the two points of the segment, separated by a '>'."));
+                }
+              else
+                {
+                  AssertThrow(temp_segment.size() == 1,ExcMessage ("The given coordinate '" + temp_segment[i_segment] + "' is not correct. "
+                                                                   "It should only contain 1 part: "
+                                                                   "the point representing the rift axis."));
+                }
+
+              // Loop over the dim-1 points of each segment (i.e. in 2d only 1 point is required for a 'segment')
+              for (unsigned int i_points = 0; i_points < dim-1; i_points++)
+                {
+                  const std::vector<double> temp_point = Utilities::string_to_double(Utilities::split_string_list(temp_segment[i_points],','));
+                  if (dim == 3)
+                    {
+                      AssertThrow(temp_point.size() == 2,ExcMessage ("The given coordinates of segment '" + temp_segment[i_points] + "' are not correct. "
+                                                                     "It should only contain 2 parts: "
+                                                                     "the two coordinates of the segment end point, separated by a ','."));
+                    }
+                  else
+                    {
+                      AssertThrow(temp_point.size() == 1,ExcMessage ("The given coordinates of segment '" + temp_segment[i_points] + "' are not correct. "
+                                                                     "It should only contain 1 part: "
+                                                                     "the one coordinate of the segment end point."));
+                    }
+
+                  // Add the point to the list of points for this segment
+                  point_list[i_segment][i_points][0] = temp_point[0];
+                  point_list[i_segment][i_points][1] = temp_point[dim-2];
+                }
+            }
+
+          // Split the string into the separate polygons
+          const std::vector<std::string> temp_polygons = Utilities::split_string_list(prm.get("Lithospheric polygons"),';');
+          const std::vector<std::string> temp_thicknesses = Utilities::split_string_list(prm.get("Lithospheric polygon layer thicknesses"),';');
+          const unsigned int n_polygons = temp_polygons.size();
+          AssertThrow(temp_thicknesses.size() == n_polygons,
+                      ExcMessage("The number of polygons (" + Utilities::int_to_string(n_polygons) +
+                                 ") does not correspond to the number of polygons for which a thickness is prescribed (" +
+                                 Utilities::int_to_string(temp_thicknesses.size()) + ")."));
+
+
+
+          polygon_point_list.resize(n_polygons);
+          polygon_thicknesses.resize(n_polygons);
+
+          for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
+            {
+              polygon_thicknesses[i_polygons] = Utilities::string_to_double(Utilities::split_string_list(temp_thicknesses[i_polygons],','));
+              AssertThrow(polygon_thicknesses[i_polygons].size()==3,
+                          ExcMessage ("The number of layer thicknesses should be equal to 3 for polygon: " + Utilities::int_to_string(i_polygons) +
+                                      " but it is " + Utilities::int_to_string(polygon_thicknesses[i_polygons].size())));
+
+//sb              std::cout << "polygon thicknesses ";
+//sb              for (unsigned int q=0; q<polygon_thicknesses[i_polygons].size(); ++q)
+//sb                std::cout << polygon_thicknesses[i_polygons][q] << " ";
+//sb              std::cout << std::endl;
+
+              // Split the string into point strings
+              const std::vector<std::string> temp_points = Utilities::split_string_list(temp_polygons[i_polygons],'>');
+              const unsigned int n_temp_points = temp_points.size();
+              if (dim == 3)
+                {
+                  AssertThrow(n_temp_points>=3, ExcMessage ("The number of polygon points should be equal to or larger than 3 in 3d."));
+                }
+              else
+                {
+                  AssertThrow(n_temp_points==2, ExcMessage ("The number of polygon points should be equal to 2 in 2d."));
+                }
+              polygon_point_list[i_polygons].resize(n_temp_points);
+              // Loop over the points of the polygon. Each point should consist of 2 values (lon and lat coordinate).
+              for (unsigned int i_points = 0; i_points < n_temp_points; i_points++)
+                {
+                  const std::vector<double> temp_point = Utilities::string_to_double(Utilities::split_string_list(temp_points[i_points],','));
+                  AssertThrow(temp_point.size() == dim-1,ExcMessage ("The given coordinates of point '" + temp_points[i_points] + "' are not correct. "
+                                                                     "It should only contain 1 (2d) or 2 (in 3d) parts: "
+                                                                     "the longitude/x (and latitude/y in 3d) coordinate (separated by a ',')."));
+
+                  // Add the point to the list of points for this segment
+                  polygon_point_list[i_polygons][i_points][0] = temp_point[0];
+                  polygon_point_list[i_polygons][i_points][1] = temp_point[dim-2];
+                }
+              if  (dim == 2)
+                AssertThrow(polygon_point_list[i_polygons][0][0] < polygon_point_list[i_polygons][1][0], ExcMessage("The order of the x coordinates of the 2 points "
+                            "of each 2d polygon should be ascending. "));
+
+            }
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+    }
+
+  }
+}
+
+// explicit instantiations
+namespace aspect
+{
+  namespace InitialComposition
+  {
+    ASPECT_REGISTER_INITIAL_COMPOSITION_MODEL(LithosphereRift,
+                                              "lithosphere with rift",
+                                              "A class that implements initial conditions for a continental rift "
+                                              "by computing the thickness of the upper crust, lower crust and mantle "
+                                              "lithosphere layers. This thickness decreases towards the axis of the "
+                                              "rift according to a Gaussian distribution whose amplitude and standard "
+                                              "deviation can be specified from the input file. "
+                                              "Additional variations in layer thicknesses can be introduced through the "
+                                              "addition of polygons. Note that the different polygons "
+                                              "are assumed not to overlap. ")
+  }
+}
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
new file mode 100644
index 00000000000..267914645ba
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
@@ -0,0 +1,147 @@
+/*
+  Copyright (C) 2017 by the authors of the ASPECT code.
+
+  This file is part of ASPECT.
+
+  ASPECT is free software; you can redistribute it and/or modify
+  it under the terms of the GNU General Public License as published by
+  the Free Software Foundation; either version 2, or (at your option)
+  any later version.
+
+  ASPECT is distributed in the hope that it will be useful,
+  but WITHOUT ANY WARRANTY; without even the implied warranty of
+  MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE.  See the
+  GNU General Public License for more details.
+
+  You should have received a copy of the GNU General Public License
+  along with ASPECT; see the file LICENSE.  If not see
+  <http://www.gnu.org/licenses/>.
+*/
+
+
+#ifndef _aspect_initial_composition_lithosphere_rift_h
+#define _aspect_initial_composition_lithosphere_rift_h
+
+#include <aspect/initial_composition/interface.h>
+#include <aspect/simulator_access.h>
+
+namespace aspect
+{
+  namespace InitialComposition
+  {
+    using namespace dealii;
+
+    /**
+     * A class that implements initial conditions for the composition
+     * considering a lithosphere consisting of an upper crust,
+     * lower crust and mantle part.
+     *
+     * @ingroup InitialCompositionModels
+     */
+    template <int dim>
+    class LithosphereRift : public Interface<dim>,
+      public SimulatorAccess<dim>
+    {
+      public:
+
+        /**
+         * Initialization function. This function is called once at the
+         * beginning of the program. Checks preconditions.
+         */
+        void
+        initialize ();
+
+        /**
+         * Return the initial composition as a function of position and number
+         * of compositional field.
+         */
+        virtual
+        double initial_composition (const Point<dim> &position,
+                                    const unsigned int compositional_index) const;
+
+        /**
+         * Return the overall shortest distance to the rift segments
+         */
+        double distance_to_rift (const Point<dim-1> &position) const;
+
+        /*
+         * Return the overall shortest distance to the polygon segments
+         */
+        std::pair<double,unsigned int> distance_to_polygon (const Point<dim-1> &position) const;
+
+        /*
+         * Return the position of the point in surface coordinates
+         * i.e. x(,y) in meters or lon(,lat) in degrees.
+         */
+        Point<dim-1> surface_position (const Point<dim> &position,
+                                       const bool cartesian_geometry) const;
+
+        /**
+         * Declare the parameters this class takes through input files.
+         */
+        static
+        void
+        declare_parameters (ParameterHandler &prm);
+
+        /**
+         * Read the parameters this class declares from the parameter file.
+         */
+        virtual
+        void
+        parse_parameters (ParameterHandler &prm);
+
+      private:
+
+        /**
+         * The standard deviation of the Gaussian amplitude of the lithospheric thicknesses
+         * with distance from the rift axis.
+         */
+        double sigma_rift;
+
+        /**
+         * The half width of the hyperbolic tangent used to smooth the transitions
+         * between reference and polygon lithospheric thicknesses.
+         */
+        double sigma_polygon;
+
+        /**
+         * Whether or not to take the polygon thicknesses as dominant, or to smooth them
+         * gradually into rift areas.
+         */
+        bool blend_rift_and_polygon;
+
+        /**
+         * The maximum amplitude of the Gaussian distribution of the lithospheric thicknesses
+         * with distance from the rift axis. It should have values between -1 and 1, where positive
+         * numbers represent a reduction in thickness and negative numbers an increase.
+         */
+        std::vector<double> A;
+
+        /**
+         * The list of line segments consisting of two 2d coordinates per segment.
+         * The segments represent the rift axis.
+         */
+        std::vector<std::array<Point<2>,2 > > point_list;
+
+        /**
+         * The list of lists of polygon points.
+         * The polygon represents an area of different lithospheric thicknesses.
+         */
+        std::vector<std::vector<Point<2> > > polygon_point_list;
+
+        /**
+         * Vector for the reference field thicknesses away from the rift.
+         */
+        std::vector<double> thicknesses;
+
+        /**
+         * Vector for the field thicknesses inside the polygons.
+         */
+        std::vector<std::vector<double> > polygon_thicknesses;
+
+    };
+  }
+}
+
+
+#endif
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
new file mode 100644
index 00000000000..954ced16112
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
@@ -0,0 +1,152 @@
+/*
+  Copyright (C) 2014 - 2016 by the authors of the ASPECT code.
+
+  This file is part of ASPECT.
+
+  ASPECT is free software; you can redistribute it and/or modify
+  it under the terms of the GNU General Public License as published by
+  the Free Software Foundation; either version 2, or (at your option)
+  any later version.
+
+  ASPECT is distributed in the hope that it will be useful,
+  but WITHOUT ANY WARRANTY; without even the implied warranty of
+  MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE.  See the
+  GNU General Public License for more details.
+
+  You should have received a copy of the GNU General Public License
+  along with ASPECT; see the file doc/COPYING.  If not see
+  <http://www.gnu.org/licenses/>.
+*/
+
+
+
+#ifndef _aspect_initial_temperature_lithosphere_rift_h
+#define _aspect_initial_temperature_lithosphere_rift_h
+
+#include <aspect/initial_temperature/interface.h>
+#include <aspect/simulator_access.h>
+
+namespace aspect
+{
+
+
+  namespace InitialTemperature
+  {
+
+    /**
+     *
+     * @ingroup InitialTemperatures
+     */
+    template <int dim>
+    class LithosphereRift : public Interface<dim>, public ::aspect::SimulatorAccess<dim>
+    {
+      public:
+        /**
+         * Constructor.
+         */
+        LithosphereRift ();
+
+        /**
+         * Initialization function. This function is called once at the
+         * beginning of the program. Checks preconditions.
+         */
+        void
+        initialize ();
+
+        /**
+         * Return the initial temperature as a function of position.
+         */
+        virtual
+        double initial_temperature (const Point<dim> &position) const;
+
+        /**
+         * Return the initial temperature as a function of depth and
+         * the local layer thicknesses.
+         */
+        virtual
+        double temperature (const double depth,
+                            const std::vector<double> thicknesses) const;
+
+        /**
+         * Declare the parameters this class takes through input files.
+         */
+        static
+        void
+        declare_parameters (ParameterHandler &prm);
+
+        /**
+         * Read the parameters this class declares from the parameter file.
+         */
+        virtual
+        void
+        parse_parameters (ParameterHandler &prm);
+
+      private:
+        /**
+         * Surface temperature
+         */
+        double T0;
+
+        /**
+         * LAB isotherm temperature
+         */
+        double LAB_isotherm;
+
+        /**
+         * Wheter or not to take the polygon thicknesses as dominant, or to smooth them
+         * gradually into rift areas.
+         */
+        bool blend_rift_and_polygon;
+
+        /**
+         * Vector for field heat production rates.
+         */
+        std::vector<double> heat_productivities;
+
+        /**
+         * Vector for thermal conductivities.
+         */
+        std::vector<double> conductivities;
+
+        /**
+         * Vector for field densities.
+         */
+        std::vector<double> densities;
+
+        /**
+         * Vector for the reference field thicknesses.
+         */
+        std::vector<double> thicknesses;
+
+        /**
+         * Vector for the reference field thicknesses away from the rift.
+         */
+        std::vector<std::vector<double> > polygon_thicknesses;
+
+        /**
+         * The standard deviation of the Gaussian amplitude of the lithospheric thicknesses.
+         */
+        double sigma_rift;
+        double sigma_polygon;
+
+        /**
+         * The maximum amplitude of the Gaussian distribution of the lithospheric thicknesses
+         * with distance from the rift axis. It should have values between -1 and 1, where positive
+         * numbers represent a reduction in thickness and negative numbers an increase.
+         */
+        std::vector<double> A;
+
+        /**
+         * Whether or not to use a compensation depth for the temperature
+         * up to which the LAB isotherm is prescribed. If yes, temperatures
+         * in the sub-lithospheric mantle are set to the LAB isotherm up
+         * to the depth held by the parameter compensation_depth.
+         */
+        bool use_compensation_depth;
+        double compensation_depth;
+    };
+  }
+}
+
+
+#endif
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
new file mode 100644
index 00000000000..8df533ac492
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -0,0 +1,320 @@
+/*
+  Copyright (C) 2011 - 2016 by the authors of the ASPECT code.
+
+  This file is part of ASPECT.
+
+  ASPECT is free software; you can redistribute it and/or modify
+  it under the terms of the GNU General Public License as published by
+  the Free Software Foundation; either version 2, or (at your option)
+  any later version.
+
+  ASPECT is distributed in the hope that it will be useful,
+  but WITHOUT ANY WARRANTY; without even the implied warranty of
+  MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE.  See the
+  GNU General Public License for more details.
+
+  You should have received a copy of the GNU General Public License
+  along with ASPECT; see the file doc/COPYING.  If not see
+  <http://www.gnu.org/licenses/>.
+*/
+
+
+#include "lithosphere_rift_IT.h"
+#include <aspect/utilities.h>
+#include "lithosphere_rift_IC.h"
+#include <aspect/geometry_model/box.h>
+#include <aspect/boundary_temperature/interface.h>
+#include <aspect/material_model/visco_plastic.h>
+#include <aspect/heating_model/interface.h>
+
+#include <cmath>
+
+namespace aspect
+{
+  namespace InitialTemperature
+  {
+    template <int dim>
+    LithosphereRift<dim>::LithosphereRift ()
+    {}
+
+
+    template <int dim>
+    void
+    LithosphereRift<dim>::
+    initialize ()
+    {
+
+      // Check that the required radioactive heating model ("compositional heating") is used
+      const std::vector<std::string> &heating_models = this->get_heating_model_manager().get_active_heating_model_names();
+      AssertThrow(std::find(heating_models.begin(), heating_models.end(), "compositional heating") != heating_models.end(),
+                  ExcMessage("The lithosphere with rift initial temperature plugin requires the compositional heating plugin."));
+
+      // Check that the required material model ("visco plastic") is used
+      //AssertThrow((dynamic_cast<MaterialModel::ViscoPlasticStrain<dim> *> (const_cast<MaterialModel::Interface<dim> *>(&this->get_material_model()))) != 0,
+      AssertThrow((dynamic_cast<MaterialModel::ViscoPlastic<dim> *> (const_cast<MaterialModel::Interface<dim> *>(&this->get_material_model()))) != 0,
+                  ExcMessage("The lithosphere with rift initial temperature plugin requires the viscoplastic material model plugin."));
+    }
+
+
+    template <int dim>
+    double
+    LithosphereRift<dim>::
+    initial_temperature (const Point<dim> &position) const
+    {
+      // Determine coordinate system
+      const bool cartesian_geometry = dynamic_cast<const GeometryModel::Box<dim> *>(&this->get_geometry_model()) != NULL ? true : false;
+
+      // Get the distance to the line segments along a path parallel to the surface
+      //InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> (const_cast<InitialComposition::Interface<dim> *>(&this->get_initial_composition()));
+
+      double distance_to_rift_axis = 1e23;
+      Point<dim-1> surface_position;
+      std::pair<double, unsigned int> distance_to_L_polygon;
+      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim> > >::const_iterator it = this->get_initial_composition_manager().get_active_initial_composition_conditions().begin();
+           it != this->get_initial_composition_manager().get_active_initial_composition_conditions().end();
+           ++it)
+        if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
+          {
+            surface_position = ic->surface_position(position, cartesian_geometry);
+            distance_to_rift_axis = ic->distance_to_rift(surface_position);
+            distance_to_L_polygon = ic->distance_to_polygon(surface_position);
+          }
+
+      // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
+      // based on the distance from the rift axis.
+      std::vector<double> local_thicknesses(3);
+      local_thicknesses[0] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][0]
+                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[0])
+                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
+                               (1.0 - A[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      local_thicknesses[1] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
+                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
+                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
+                               (1.0 - A[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      local_thicknesses[2] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
+                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
+                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
+                               (1.0 - A[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+
+      const double depth = this->get_geometry_model().depth(position);
+
+      return temperature(depth, local_thicknesses);
+    }
+
+
+    template <int dim>
+    double
+    LithosphereRift<dim>::
+    temperature (const double depth,
+                 const std::vector<double> layer_thicknesses) const
+    {
+      // Compute some constants
+      const double a = 0.5*densities[0]*heat_productivities[0]*layer_thicknesses[0] + 0.5*densities[1]*heat_productivities[1]*layer_thicknesses[1] + conductivities[0]/layer_thicknesses[0]*T0;
+      const double b = 1./(conductivities[0]/layer_thicknesses[0]+conductivities[1]/layer_thicknesses[1]);
+      const double c = 0.5*densities[1]*heat_productivities[1]*layer_thicknesses[1] + conductivities[2]/layer_thicknesses[2]*LAB_isotherm;
+      const double d = 1./(conductivities[1]/layer_thicknesses[1]+conductivities[2]/layer_thicknesses[2]);
+
+      //Temperature at boundary between layer 1 and 2
+      const double T1 = (a*b + conductivities[1]/layer_thicknesses[1]*c*d*b) / (1.-(conductivities[1]*conductivities[1])/(layer_thicknesses[1]*layer_thicknesses[1])*d*b);
+      //Temperature at boundary between layer 2 and 3
+      const double T2 = (c + conductivities[1]/layer_thicknesses[1]*T1) * d;
+
+      // Temperature in layer 1
+      if (depth < layer_thicknesses[0])
+        return -0.5*densities[0]*heat_productivities[0]/conductivities[0]*std::pow(depth,2) + (0.5*densities[0]*heat_productivities[0]*layer_thicknesses[0]/conductivities[0] + (T1-T0)/layer_thicknesses[0])*depth + T0;
+      // Temperature in layer 2
+      else if (depth < layer_thicknesses[0]+layer_thicknesses[1])
+        return -0.5*densities[1]*heat_productivities[1]/conductivities[1]*std::pow(depth-layer_thicknesses[0],2.) + (0.5*densities[1]*heat_productivities[1]*layer_thicknesses[1]/conductivities[1] + (T2-T1)/layer_thicknesses[1])*(depth-layer_thicknesses[0]) + T1;
+      // Temperature in layer 3
+      else if (depth < layer_thicknesses[0]+layer_thicknesses[1]+layer_thicknesses[2])
+        return (LAB_isotherm-T2)/layer_thicknesses[2] *(depth-layer_thicknesses[0]-layer_thicknesses[1]) + T2;
+      // Return a constant sublithospheric temperature of .
+      // This way we can combine the continental geotherm with an adiabatic profile from the input file
+      // using the "if valid" operator on the "List of initial temperature models"
+      else if (use_compensation_depth && depth < compensation_depth)
+        return LAB_isotherm;
+      else
+        return std::numeric_limits<double>::quiet_NaN();
+    }
+
+
+    template <int dim>
+    void
+    LithosphereRift<dim>::declare_parameters (ParameterHandler &prm)
+    {
+      prm.enter_subsection ("Initial temperature model");
+      {
+        prm.enter_subsection("Lithosphere with rift");
+        {
+
+          prm.declare_entry ("Surface temperature", "273.15",
+                             Patterns::Double (0),
+                             "The value of the surface temperature. Units: Kelvin.");
+          prm.declare_entry ("LAB isotherm temperature", "1673.15",
+                             Patterns::Double (0),
+                             "The value of the isothermal boundary temperature assumed at the LAB "
+                             "and up to the reference depth . Units: Kelvin.");
+          prm.declare_entry ("Use temperature compensation depth", "false",
+                             Patterns::Bool (),
+                             "Whether or not to use a compensation depth to which the LAB isotherm temperature "
+                             "is prescribed when no lithosphere is present. Below this depth, 10 times the isotherm "
+                             "is prescribed . Units: -.");
+          prm.declare_entry ("Temperature compensation depth", "100e3",
+                             Patterns::Double (0),
+                             "The depth of the temperature compensation depth, "
+                             "i.e. the depth up to which the LAB isotherm is prescribed when not in the lithosphere. Units: Kelvin.");
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+    }
+
+
+
+    template <int dim>
+    void
+    LithosphereRift<dim>::parse_parameters (ParameterHandler &prm)
+    {
+      unsigned int n_fields = 0;
+      prm.enter_subsection ("Compositional fields");
+      {
+        n_fields = prm.get_integer ("Number of fields");
+      }
+      prm.leave_subsection();
+
+      prm.enter_subsection ("Initial composition model");
+      {
+        prm.enter_subsection("Lithosphere with rift");
+        {
+          sigma_rift           = prm.get_double ("Standard deviation of Gaussian rift geometry");
+          sigma_polygon        = prm.get_double ("Half width of polygon smoothing");
+          blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
+          A                    = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
+                                                                         3,
+                                                                         "Amplitude of Gaussian rift geometry");
+          thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
+                                                                3,
+                                                                "Layer thicknesses");
+          // Split the string into the separate polygons
+          const std::vector<std::string> temp_thicknesses = Utilities::split_string_list(prm.get("Lithospheric polygon layer thicknesses"),';');
+          const unsigned int n_polygons = temp_thicknesses.size();
+          polygon_thicknesses.resize(n_polygons);
+          for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
+            {
+              polygon_thicknesses[i_polygons] = Utilities::string_to_double(Utilities::split_string_list(temp_thicknesses[i_polygons],','));
+              AssertThrow(polygon_thicknesses[i_polygons].size()==3, ExcMessage ("The number of layer thicknesses should be equal to 3."));
+            }
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+
+      prm.enter_subsection ("Initial temperature model");
+      {
+        prm.enter_subsection("Lithosphere with rift");
+        {
+          LAB_isotherm = prm.get_double ("LAB isotherm temperature");
+          T0 = prm.get_double ("Surface temperature");
+          use_compensation_depth = prm.get_bool ("Use temperature compensation depth");
+          compensation_depth = prm.get_double ("Temperature compensation depth");
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+
+
+      // Retrieve the indices of the fields that represent the lithospheric layers.
+      AssertThrow(this->introspection().compositional_name_exists("upper"),ExcMessage("We need a compositional field called 'upper' representing the upper crust."));
+      AssertThrow(this->introspection().compositional_name_exists("lower"),ExcMessage("We need a compositional field called 'lower' representing the lower crust."));
+      AssertThrow(this->introspection().compositional_name_exists("mantle_L"),ExcMessage("We need a compositional field called 'mantle_L' representing the lithospheric part of the mantle."));
+
+      // For now, we assume a 3-layer system with an upper crust, lower crust and lithospheric mantle
+      const unsigned int id_upper = this->introspection().compositional_index_for_name("upper");
+      const unsigned int id_lower = this->introspection().compositional_index_for_name("lower");
+      const unsigned int id_mantle_L = this->introspection().compositional_index_for_name("mantle_L");
+
+      // Retrieve other material properties set in different sections such that there
+      // is no need to set them twice.
+
+      prm.enter_subsection("Heating model");
+      {
+        prm.enter_subsection("Compositional heating");
+        {
+          // The heating model compositional heating prefixes an entry for the background material
+          const std::vector<double> temp_heat_productivities = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Compositional heating values"))),
+                                                               n_fields+1,
+                                                               "Compositional heating values");
+          // This sets the heat productivity in W/m3 units
+          heat_productivities.push_back(temp_heat_productivities[id_upper+1]);
+          heat_productivities.push_back(temp_heat_productivities[id_lower+1]);
+          heat_productivities.push_back(temp_heat_productivities[id_mantle_L+1]);
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+
+      prm.enter_subsection("Material model");
+      {
+        prm.enter_subsection("Visco Plastic");
+        {
+          // The material model viscoplastic prefixes an entry for the background material
+          const std::vector<double> temp_densities = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Densities"))),
+                                                     n_fields+1,
+                                                     "Densities");
+          const std::vector<double> temp_thermal_diffusivities = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Thermal diffusivities"))),
+                                                                 n_fields+1,
+                                                                 "Thermal diffusivities");
+          const std::vector<double> temp_heat_capacities = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Heat capacities"))),
+                                                           n_fields+1,
+                                                           "Heat capacities");
+
+          densities.push_back(temp_densities[id_upper+1]);
+          densities.push_back(temp_densities[id_lower+1]);
+          densities.push_back(temp_densities[id_mantle_L+1]);
+
+          // Thermal diffusivity kappa = k/(rho*cp), so thermal conducitivity k = kappa*rho*cp
+          conductivities.push_back(temp_thermal_diffusivities[id_upper+1] * densities[0] * temp_heat_capacities[id_upper+1]);
+          conductivities.push_back(temp_thermal_diffusivities[id_lower+1] * densities[1] * temp_heat_capacities[id_lower+1]);
+          conductivities.push_back(temp_thermal_diffusivities[id_mantle_L+1] * densities[2] * temp_heat_capacities[id_mantle_L+1]);
+
+          // To obtain the radioactive heating rate in W/kg, we divide the volumetric heating rate by density
+          AssertThrow(heat_productivities.size() == 3 && densities.size() == 3 && conductivities.size() == 3,
+                      ExcMessage("The entries for density, conductivity and heat production do not match with the expected number of layers (3)."))
+
+          for (unsigned int i = 0; i<3; ++i)
+            heat_productivities[i] /= densities[i];
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+    }
+  }
+
+
+}
+
+
+
+
+// explicit instantiations
+namespace aspect
+{
+  namespace InitialTemperature
+  {
+    ASPECT_REGISTER_INITIAL_TEMPERATURE_MODEL(LithosphereRift,
+                                              "lithosphere with rift",
+                                              "This is a temperature initial condition that "
+                                              "computes a continental geotherm based on the "
+                                              "conductive equations of Turcotte and Schubert Ch. 4.6. "
+                                              "The geotherm can be computed for any number of crustal "
+                                              "layers, for each of which a density, heat production and thermal "
+                                              "conductivity should be supplied. "
+                                              "Make sure the top and bottom temperatures of the lithosphere "
+                                              "agree with temperatures set in for example the temperature "
+                                              "boundary conditions. "
+                                              "The thickness of the lithospheric layers is adapted for distance "
+                                              "to the rift specified with the InitialComposition plugin `lithosphere "
+                                              "with rift'. Additional variations in lithospheric thickness can be "
+                                              "added through specifying polygonal areas of different thicknesses. ")
+  }
+}
diff --git a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
new file mode 100644
index 00000000000..e93162f67fa
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
@@ -0,0 +1,341 @@
+/*
+  Copyright (C) 2011 - 2016 by the authors of the ASPECT code.
+
+  This file is part of ASPECT.
+
+  ASPECT is free software; you can redistribute it and/or modify
+  it under the terms of the GNU General Public License as published by
+  the Free Software Foundation; either version 2, or (at your option)
+  any later version.
+
+  ASPECT is distributed in the hope that it will be useful,
+  but WITHOUT ANY WARRANTY; without even the implied warranty of
+  MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE.  See the
+  GNU General Public License for more details.
+
+  You should have received a copy of the GNU General Public License
+  along with ASPECT; see the file doc/COPYING.  If not see
+  <http://www.gnu.org/licenses/>.
+ */
+
+
+#include "rift_box_initial_plastic_strain.h"
+#include <aspect/postprocess/interface.h>
+#include <aspect/geometry_model/box.h>
+#include <aspect/material_model/visco_plastic.h>
+#include <aspect/utilities.h>
+
+namespace aspect
+{
+  namespace InitialComposition
+  {
+    template <int dim>
+    RiftBoxInitialPlasticStrain<dim>::RiftBoxInitialPlasticStrain ()
+    {}
+
+    template <int dim>
+    void
+    RiftBoxInitialPlasticStrain<dim>::initialize ()
+    {
+      AssertThrow(Plugins::plugin_type_matches<MaterialModel::ViscoPlastic<dim> >(this->get_material_model()),
+                  ExcMessage("This initial condition only makes sense in combination with the visco_plastic material model."));
+
+
+      // From shear_bands.cc
+      Point<dim> extents_max;
+      TableIndices<dim> size_idx;
+      for (unsigned int d=0; d<dim; ++d)
+        size_idx[d] = grid_intervals[d]+1;
+
+      Table<dim,double> white_noise;
+      white_noise.TableBase<dim,double>::reinit(size_idx);
+
+      // Max of each direction (m)
+      extents_max = extents + origin;
+
+      // Add initial topography to vertical direction
+      extents_max[dim-1] += maximum_initial_topography;
+
+      for (unsigned int d=0; d<dim; ++d)
+        {
+          grid_extents[d].first=origin[d];
+          grid_extents[d].second=extents_max[d];
+        }
+
+      // use a fixed number as seed for random generator
+      // this is important if we run the code on more than 1 processor
+      std::srand(seed);
+
+      TableIndices<dim> idx;
+
+      for (unsigned int i=0; i<white_noise.size()[0]; ++i)
+        {
+          idx[0] = i;
+          for (unsigned int j=0; j<white_noise.size()[1]; ++j)
+            {
+              idx[1] = j;
+              if (dim == 3)
+                {
+                  for (unsigned int k=0; k<white_noise.size()[dim-1]; ++k)
+                    {
+                      idx[dim-1] = k;
+                      // std::rand will give a value between zero and RAND_MAX (usually INT_MAX).
+                      // The modulus of this value and 10000, gives a value between 0 and 10000-1.
+                      // Subsequently dividing by 5000.0 will give value between 0 and 2 (excluding 2).
+                      // Subtracting 1 will give a range [-1,1)
+                      // Because we want values [0,1), we change our white noise computation to:
+                      white_noise(idx) = ((std::rand() % 10000) / 10000.0);
+                    }
+                }
+              else
+                white_noise(idx) = ((std::rand() % 10000) / 10000.0);
+            }
+        }
+
+      interpolate_noise = new Functions::InterpolatedUniformGridData<dim> (grid_extents,
+                                                                           grid_intervals,
+                                                                           white_noise);
+    }
+
+    template <int dim>
+    double
+    RiftBoxInitialPlasticStrain<dim>::
+    initial_composition (const Point<dim> &position, const unsigned int n_comp) const
+    {
+      // If n_comp does not represent the strain field,
+      // return 0 right away.
+      if (n_comp != strain_composition_number)
+        return 0.0;
+
+      // Initiate distance with large value
+      double distance_to_rift_axis = 1e23;
+      double temp_distance = 0;
+
+      const Point<dim> natural_coords = position;
+
+      // Loop over all line segments
+      for (unsigned int i_segments = 0; i_segments < point_list.size(); ++i_segments)
+        {
+          if (dim == 2)
+            temp_distance = std::abs(natural_coords[0]-point_list[i_segments][0][0]);
+          else
+            {
+              // Get the surface coordinates by dropping the last coordinate
+              const Point<2> surface_position = Point<2>(natural_coords[0],natural_coords[1]);
+              temp_distance = std::abs(Utilities::distance_to_line(point_list[i_segments], surface_position));
+            }
+
+          // Get the minimum distance
+          distance_to_rift_axis = std::min(distance_to_rift_axis, temp_distance);
+        }
+
+      // Smoothing of noise with height (depth with respect to the unperturbed surface)
+      const double depth_smoothing = 0.5 * (1.0 + std::tanh((position[dim-1] - strain_height) / strain_halfwidth));
+      // Smoothing of noise with lateral distance to the rift axis
+      const double noise_amplitude = A * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma,2)))) * depth_smoothing;
+
+      // Add randomness
+      return noise_amplitude * interpolate_noise->value(natural_coords);
+    }
+
+    template <int dim>
+    void
+    RiftBoxInitialPlasticStrain<dim>::declare_parameters (ParameterHandler &prm)
+    {
+      prm.enter_subsection("Initial composition model");
+      {
+        prm.enter_subsection("Rift box initial plastic strain");
+        {
+          prm.declare_entry ("Random number generator seed", "0",
+                             Patterns::Double (0),
+                             "The value of the seed used for the random number generator. "
+                             "Units: none.");
+          prm.declare_entry ("Standard deviation of Gaussian noise amplitude distribution", "20000",
+                             Patterns::Double (0),
+                             "The standard deviation of the Gaussian distribution of the amplitude of the strain noise. "
+                             "Note that this parameter is taken to be the same for all rift segments. "
+                             "Units: $m$ or degrees.");
+          prm.declare_entry ("Maximum amplitude of Gaussian noise amplitude distribution", "0.2",
+                             Patterns::Double (0),
+                             "The amplitude of the Gaussian distribution of the amplitude of the strain noise. "
+                             "Note that this parameter is taken to be the same for all rift segments. "
+                             "Units: none.");
+          prm.declare_entry ("Depth around which Gaussian noise is smoothed out", "40000",
+                             Patterns::Double (0),
+                             "The depth around which smoothing out of the strain noise starts with a hyperbolic tangent. "
+                             "Note that this parameter is taken to be the same for all rift segments. Also, depth "
+                             "is with respect to the unperturbed surface of the box domain. "
+                             "Units: $m$.");
+          prm.declare_entry ("Halfwidth with which Gaussian noise is smoothed out in depth", "40000",
+                             Patterns::Double (0),
+                             "The halfwidth with which smoothing out of the strain noise is done with a hyperbolic tangent. "
+                             "Note that this parameter is taken to be the same for all rift segments. "
+                             "Units: $m$.");
+          prm.declare_entry ("Rift axis line segments",
+                             "",
+                             Patterns::Anything(),
+                             "Set the line segments that represent the rift axis. In 3d each segment is made up of "
+                             "two points that represent horizontal coordinates (x,y). "
+                             "The exact format for the point list describing the segments is "
+                             "\"x1,y1>x2,y2;x2,y2>x3,y3;x4,y4>x5,y5\". In 2d, a segment is made up by 1 horizontal "
+                             "x coordinate: \"x1;x2;x3\". Note that the segments can be connected "
+                             "or isolated. Units: $m$.");
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+    }
+
+
+    template <int dim>
+    void
+    RiftBoxInitialPlasticStrain<dim>::parse_parameters (ParameterHandler &prm)
+    {
+      // Check that there is a compositional field called strain and retrieve its index
+      AssertThrow(this->introspection().compositional_name_exists("plastic_strain"),
+                  ExcMessage("This plugin requires a compositional field named plastic_strain. "));
+      strain_composition_number = this->introspection().compositional_index_for_name("plastic_strain");
+
+      AssertThrow(Plugins::plugin_type_matches<GeometryModel::Box<dim> >(this->get_geometry_model()),
+                  ExcMessage("This initial condition only makes sense in combination with the box geometry model."));
+
+      // Get the number of mesh cells in each direction
+      prm.enter_subsection("Geometry model");
+      {
+        prm.enter_subsection("Box");
+        {
+          origin[0] = prm.get_double ("Box origin X coordinate");
+          extents[0] = prm.get_double ("X extent");
+          repetitions[0] = prm.get_integer ("X repetitions");
+          origin[1] = prm.get_double ("Box origin Y coordinate");
+          extents[1] = prm.get_double ("Y extent");
+          repetitions[1] = prm.get_integer ("Y repetitions");
+          if (dim >= 3)
+            {
+              origin[dim-1] = prm.get_double ("Box origin Z coordinate");
+              extents[dim-1] = prm.get_double ("Z extent");
+              repetitions[dim-1] = prm.get_integer ("Z repetitions");
+            }
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+
+      unsigned int refinement;
+      prm.enter_subsection("Mesh refinement");
+      {
+        refinement = prm.get_integer("Initial adaptive refinement") + prm.get_integer("Initial global refinement");
+      }
+      prm.leave_subsection();
+
+      // The grid intervals equal the number of mesh cells.
+      for (unsigned int d = 0; d < dim; ++d)
+        grid_intervals[d] = repetitions[d] * std::pow(2, refinement);
+
+      // Both initial mesh deformation and initial topography models
+      // can distort the initial mesh such that the vertical coordinate
+      // of some locations is larger than the initial, unperturbed,
+      // vertical extent of the model domain. Since not all initial topography
+      // models (correctly) return a maximum topography, and
+      // initial mesh deformation models do not at all, we here assume
+      // a maximal initial topography of 10 km. This is added to the
+      // vertical extent.
+      //
+      // In the vertical direction, we add enough grid cells
+      // to cover 10 km at the same resolution. Round up the number of cells.
+      grid_intervals[dim-1] += static_cast<int>(std::ceil(maximum_initial_topography / (extents[dim-1] / grid_intervals[dim-1])));
+
+      this->get_pcout() << "Max initial topo: " << maximum_initial_topography << std::endl;
+      this->get_pcout() << "Grid intervals X: " << grid_intervals[0] << std::endl;
+      this->get_pcout() << "Grid intervals Y: " << grid_intervals[dim-1] << std::endl;
+
+      prm.enter_subsection("Initial composition model");
+      {
+        prm.enter_subsection("Rift box initial plastic strain");
+        sigma                = prm.get_double ("Standard deviation of Gaussian noise amplitude distribution");
+        A                    = prm.get_double ("Maximum amplitude of Gaussian noise amplitude distribution");
+        seed                 = prm.get_double ("Random number generator seed");
+        strain_height        = origin[dim-1] + extents[dim-1] - prm.get_double ("Depth around which Gaussian noise is smoothed out");
+        strain_halfwidth     = prm.get_double ("Halfwidth with which Gaussian noise is smoothed out in depth");
+
+        // Read in the string of rift segments
+        const std::string temp_all_segments = prm.get("Rift axis line segments");
+        // Split the string into segment strings
+        const std::vector<std::string> temp_segments = Utilities::split_string_list(temp_all_segments,';');
+        // The number of segments, each consisting of a begin and an end point in 3d and one point in 3d
+        const unsigned int n_temp_segments = temp_segments.size();
+        point_list.resize(n_temp_segments);
+
+        // Loop over the segments to extract the points
+        for (unsigned int i_segment = 0; i_segment < n_temp_segments; i_segment++)
+          {
+            // In 3d a line segment consists of 2 points,
+            // in 2d of only 1 (ridge axis orthogonal to x and y).
+            // Also, a 3d point has 2 coordinates (x and y),
+            // a 2d point only 1 (x).
+            const std::vector<std::string> temp_segment = Utilities::split_string_list(temp_segments[i_segment],'>');
+
+            if (dim == 3)
+              {
+                // const std::vector<std::string> temp_segment = Utilities::split_string_list(temp_segments[i_segment],'>');
+                AssertThrow(temp_segment.size() == 2,ExcMessage ("The given coordinate '" + temp_segment[i_segment] + "' is not correct. "
+                                                                 "It should only contain 2 parts: "
+                                                                 "the two points of the segment, separated by a '>'."));
+
+              }
+            else
+              {
+                // Add the point to the list of points for this segment
+                // As we're in 2d all segments correspond to 1 point consisting of 1 coordinate
+                AssertThrow(temp_segment.size() == 1,ExcMessage ("The given coordinate '" + temp_segment[i_segment] + "' is not correct. "
+                                                                 "It should only contain 1 part: "
+                                                                 "the point representing the rift axis."));
+              }
+
+            // Loop over the 2 points of each segment
+            for (unsigned int i_points = 0; i_points < dim-1; i_points++)
+              {
+                std::vector<double> temp_point = Utilities::string_to_double(Utilities::split_string_list(temp_segment[i_points],','));
+                if (dim == 3)
+                  {
+                    AssertThrow(temp_point.size() == 2,ExcMessage ("The given coordinates of segment '" + temp_segment[i_points] + "' are not correct. "
+                                                                   "It should only contain 2 parts: "
+                                                                   "the x and y coordinates of the segment begin/end point, separated by a ','."));
+                  }
+                else
+                  {
+                    AssertThrow(temp_point.size() == 1,ExcMessage ("The given coordinates of segment '" + temp_segment[i_points] + "' are not correct. "
+                                                                   "It should only contain 1 part: "
+                                                                   "the one coordinate of the segment end point."));
+                  }
+
+                // Add the point to the list of points for this segment
+                point_list[i_segment][i_points][0] = temp_point[0];
+                point_list[i_segment][i_points][1] = temp_point[dim-2];
+              }
+          }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+    }
+
+  }
+}
+
+// explicit instantiations
+namespace aspect
+{
+  namespace InitialComposition
+  {
+    ASPECT_REGISTER_INITIAL_COMPOSITION_MODEL(RiftBoxInitialPlasticStrain,
+                                              "rift box initial plastic strain",
+                                              "Specify the plastic strain initial compositional field value based on "
+                                              "the distance to a list of line segments "
+                                              "and the user-defined Gaussian distribution around these segments, "
+                                              "combined with random noise. "
+                                              "A maximum initial topography of 10 km can be accommodated. Initial topography that "
+                                              "is higher than 10 km will lead to plastic strain values set to the strain value at 10 km."
+                                              "This plugin only works in combination with the box geometry model and the visco_plastic "
+                                              "material model.")
+  }
+}
diff --git a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
new file mode 100644
index 00000000000..6003e0c26ab
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
@@ -0,0 +1,162 @@
+/*
+  Copyright (C) 2011 - 2016 by the authors of the ASPECT code.
+
+  This file is part of ASPECT.
+
+  ASPECT is free software; you can redistribute it and/or modify
+  it under the terms of the GNU General Public License as published by
+  the Free Software Foundation; either version 2, or (at your option)
+  any later version.
+
+  ASPECT is distributed in the hope that it will be useful,
+  but WITHOUT ANY WARRANTY; without even the implied warranty of
+  MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE.  See the
+  GNU General Public License for more details.
+
+  You should have received a copy of the GNU General Public License
+  along with ASPECT; see the file doc/COPYING.  If not see
+  <http://www.gnu.org/licenses/>.
+*/
+
+
+#ifndef _aspect_initial_composition_rift_box_initial_plastic_strain_h
+#define _aspect_initial_composition_rift_box_initial_plastic_strain_h
+
+#include <aspect/initial_composition/interface.h>
+#include <aspect/simulator_access.h>
+
+#include <deal.II/base/function_lib.h>
+
+namespace aspect
+{
+  namespace InitialComposition
+  {
+    using namespace dealii;
+
+    /**
+     * A class that implements initial conditions for the compositional fields
+     * based on a functional description provided in the input file.
+     *
+     * @ingroup InitialCompositionModels
+     */
+    template <int dim>
+    class RiftBoxInitialPlasticStrain : public Interface<dim>,
+      public SimulatorAccess<dim>
+    {
+      public:
+        /**
+         * Constructor.
+         */
+        RiftBoxInitialPlasticStrain ();
+
+        /**
+         * Initialization function.
+         */
+        void
+        initialize ();
+
+        /**
+         * Return the initial composition as a function of position and number
+         * of compositional field. The composition varies as a Gaussian distribution
+         * around a user-defined set of line-segments.
+         */
+        virtual
+        double initial_composition (const Point<dim> &position, const unsigned int n_comp) const;
+
+        /**
+         * Declare the parameters this class takes through input files. The
+         * default implementation of this function does not describe any
+         * parameters. Consequently, derived classes do not have to overload
+         * this function if they do not take any runtime parameters.
+         */
+        static
+        void
+        declare_parameters (ParameterHandler &prm);
+
+        /**
+         * Read the parameters this class declares from the parameter file.
+         * The default implementation of this function does not read any
+         * parameters. Consequently, derived classes do not have to overload
+         * this function if they do not take any runtime parameters.
+         */
+        virtual
+        void
+        parse_parameters (ParameterHandler &prm);
+
+      private:
+
+        /**
+         * The number of the compositional field representing the strain.
+         */
+        unsigned int strain_composition_number;
+
+        /**
+         * The value of the seed for the random number generator
+         */
+        double seed;
+
+        /**
+         * The maximum amplitude of the Gaussian amplitude of the noise.
+         */
+        double A;
+
+        /**
+         * The standard deviation of the Gaussian amplitude of the noise.
+         */
+        double sigma;
+
+        /**
+         * The height around and halfwidth with which the noise is smoothed out.
+         */
+        double strain_height;
+        double strain_halfwidth;
+
+        /**
+         * The list of line segments consisting of two 2d coordinates per segment (even in 2d).
+         * The segments represent the rift axis.
+         */
+        std::vector<std::array<Point<2>,2 > > point_list;
+
+        /**
+         * A table with random noise for the
+         * second invariant of the strain.
+         */
+        std::array<unsigned int,dim> grid_intervals;
+        Functions::InterpolatedUniformGridData<dim> *interpolate_noise;
+
+        /**
+         * A pointer to the initial topography model.
+         */
+        InitialTopographyModel::Interface<dim> *topo_model;
+
+        /**
+         * The min and max of the strain grid in each direction
+         */
+        std::array<std::pair<double,double>,dim> grid_extents;
+
+        /**
+         * Origin of the box in x, y, and z (in 3d) coordinates.
+         */
+        Point<dim> origin;
+
+        /**
+         * Extent of the domain in x-, y-, and z-direction (in 3d).
+         */
+        Point<dim> extents;
+
+        /**
+         * The number of cells in each coordinate direction (x, y, z).
+         */
+        std::array<unsigned int, dim> repetitions;
+
+        /**
+         * The height we add to vertical domain extent
+         * to deal with any initial topography.
+         */
+        const double maximum_initial_topography = 5000.;
+    };
+  }
+}
+
+
+#endif

From 8729e67cff1988949e3b2230ebfccb6769702a40 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Tue, 12 Dec 2023 12:31:48 +0100
Subject: [PATCH 02/38] First stab prm file

---
 .../initial_conditions_continental_rift.prm   | 328 ++++++++++++++++++
 1 file changed, 328 insertions(+)
 create mode 100644 cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm

diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
new file mode 100644
index 00000000000..40cc2cfeca6
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
@@ -0,0 +1,328 @@
+#### Continental Extension Cookbook
+# This cookbook is based off numerous published studies, five of which are listed below.
+# For additional information, see these publications and references therein.
+#   1. Brune, S., Heine, C., Perez-Gussinye, M., and Sobolev, S.V. (2014), Nat. Comm., v.5, n.4014,
+#      Rift migration explains continental margin asymmetry and crustal hyperextension
+#   2. Huismans, R., and Beaumont, C. (2011), Nature, v.473, p.71-75.
+#      Depth-dependent extension, two-stage breakup and cratonic underplating at rifted margins
+#   3. Naliboff, J., and Buiter, S.H. (2015), Earth Planet. Sci. Lett., v.421, p.58-67,
+#      "Rift Reactivation and migration during multiphase extension"
+#   4. Naliboff, J., Glerum, A., Sascha, S., Peron-Pinvidic, G., and Wrona, T. (2020), Geophys.
+#      Res. Lett., 47, e2019GL086611, "Development of 3‐D rift heterogeneity through fault
+#      network evolution"
+#   5. Sandiford, D., Brune, S., Glerum, A., Naliboff, J., and Whittaker, J.M. (2021), Geophys.
+#      Geochem. Geosys., 22, e2021GC009681, "Kinematics of footwall exhumation at oceanic
+#      detachment faults: Solid-block rotation and apparent unbending"
+
+####  Global parameters
+set Additional shared libraries            = /Applications/ASPECT/VisualStudioCode/aspect/cookbooks/initial_conditions_continental_rift/libinitial_conditions_continental_rift.debug.so
+set Dimension                              = 2
+set Start time                             = 0
+set End time                               = 5e6
+set Use years in output instead of seconds = true
+set Nonlinear solver scheme                = single Advection, iterated defect correction Stokes
+set Nonlinear solver tolerance             = 1e-4
+set Max nonlinear iterations               = 100
+set CFL number                             = 0.5
+set Maximum time step                      = 20e3
+set Output directory                       = output-continental_extension
+set Pressure normalization                 = no
+
+#### Parameters describing the model
+
+# Governing equations
+subsection Formulation
+  set Formulation = Boussinesq approximation
+end
+
+# Model geometry (200x100 km, 20 km spacing)
+subsection Geometry model
+  set Model name = box
+
+  subsection Box
+    set X repetitions = 10
+    set Y repetitions = 5
+    set X extent      = 200e3
+    set Y extent      = 100e3
+  end
+end
+
+# Globally refine the mesh to 2.5 km spacing, and then
+# adaptively refine the mesh to 1.25 km spacing above y=50 km
+# and between x=40 and x=160 km. These values ensure areas
+# undergoing brittle deformation are in the high-resolution
+# region.
+subsection Mesh refinement
+  set Initial adaptive refinement        = 1
+  set Initial global refinement          = 3
+  set Time steps between mesh refinement = 0
+  set Strategy = minimum refinement function
+
+  subsection Minimum refinement function
+    set Coordinate system   = cartesian
+    set Variable names      = x,y
+    set Function expression = if ( y>=50e3 && x>=40.e3 && x<=160.e3, 4, 3)
+  end
+end
+
+# Use the Eisenstat Walker method to automatically determine the
+# linear solver tolerance during the defect Picard iterations.
+# Adjusting the Maximum linear solver tolerance will affect how long
+# it takes to reach a solution, but not the actual value of the
+# solution.
+subsection Solver parameters
+  subsection Stokes solver parameters
+    set Number of cheap Stokes solver steps = 0
+  end
+
+  subsection Newton solver parameters
+    set Maximum linear Stokes solver tolerance   = 1e-2
+    set Use Eisenstat Walker method for Picard iterations = true
+  end
+end
+
+# Advecting the free surface using a normal, rather than vertical,
+# projection. To reduce mesh instabilities and associated solver
+# issues when deformation becomes large, diffusion is applied to
+# the free surface at each time step.
+subsection Mesh deformation
+  set Mesh deformation boundary indicators        = top: free surface, top: diffusion
+
+  subsection Free surface
+    set Surface velocity projection = normal
+  end
+
+  subsection Diffusion
+    # Diffusivity term. Increasing this value will result
+    # in a smoother free surface and lower topography
+    # amplitudes.
+    set Hillslope transport coefficient = 1.e-8
+  end
+end
+
+# Velocity on boundaries characterized by functions
+# The outward velocity (x-direction) on the left and right walls is 0.25 cm/year
+# The vertical velocity at the base is 0.25 cm/year (balances outflow on sides)
+# Velocity components parallel to the base (x-velocity) and side walls (y-velocity)
+# are unconstrained (i.e. 'free').
+subsection Boundary velocity model
+  set Prescribed velocity boundary indicators = left x: function, right x:function, bottom y:function
+
+  subsection Function
+    set Variable names      = x,y
+    set Function constants  = v=0.0025, w=200.e3, d=100.e3
+    set Function expression = if (x < w/2 , -v, v) ; v*2*d/w
+  end
+end
+
+# Number and names of compositional fields
+# The five compositional fields represent:
+# 1. The plastic strain that accumualates over time, with the initial plastic strain removed
+# 2. The plastic strain that accumulated over time, including the initial plastic strain values
+# 3. The upper crust
+# 4. The lower crust
+# 5. The mantle lithosphere
+subsection Compositional fields
+  set Number of fields = 5
+  set Names of fields = noninitial_plastic_strain, plastic_strain, upper_crust, lower_crust, mantle_lithosphere
+end
+
+# Initial values of different compositional fields
+# The upper crust (20 km thick), lower crust (20 km thick)
+# and mantle (60 km thick) are continuous horizontal layers
+# of constant thickness. The non initial plastic strain is set
+# to 0 and the initial plastic strain is randomized between
+# 0.5 and 1.5.
+subsection Initial composition model
+  set List of model names = function, rift box initial plastic strain #lithosphere with rift
+#  subsection Lithosphere with rift
+#    set Blend polygons and rifts                       = true
+#    set Standard deviation of Gaussian rift geometry   = 60e3
+#    set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
+    # LAB at 110 km
+#    set Rift axis line segments                        = 350e3  
+#    set Layer thicknesses                              = 20e3, 15e3, 85e3
+   
+    # Polygon LAB at 200 km
+#    set Lithospheric polygon layer thicknesses         = 23e3, 20e3 , 157.e3
+#    set Lithospheric polygons                          = 450e3 > 3000e3
+#    set Half width of polygon smoothing                = 10e3 
+#  end
+
+  subsection Function
+    set Variable names      = x,y
+    set Function expression = 0; \
+                              if(x>50.e3 && x<150.e3 && y>50.e3, 0.5 + rand_seed(1), 0); \
+                              if(y>=80.e3, 1, 0); \
+                              if(y<80.e3 && y>=60.e3, 1, 0); \
+                              if(y<60.e3, 1, 0);
+  end
+end
+
+# Composition: fixed on bottom (inflow boundary), free on sides and top
+subsection Boundary composition model
+  set Fixed composition boundary indicators = bottom
+  set List of model names = initial composition
+end
+
+# Temperature boundary conditions
+# Top and bottom (fixed) temperatures are consistent with the initial temperature field
+# Note that while temperatures are specified for the model sides, these values are
+# not used as the sides are not specified "Fixed temperature boundaries".  Rather,
+# these boundaries are insulating (zero net heat flux).
+subsection Boundary temperature model
+  set Fixed temperature boundary indicators = bottom, top
+  set List of model names = box
+
+  subsection Box
+    set Bottom temperature = 1613
+    set Top temperature    =  273
+  end
+end
+
+# Initial temperature field
+# Typical continental geotherm based on equations 4-6 from:
+#   D.S. Chapman (1986), "Thermal gradients in the continental crust",
+#   Geological Society of London Special Publications, v.24, p.63-70.
+# The initial constraints are:
+#   Surface Temperature  - upper crust (ts1) = 273 K
+#   Surface Heat Flow    - upper crust (qs1) = 0.055 mW/m^2
+#   Heat Production      - upper crust (A1)  = 1.00e-6 W/m^3;
+#   Heat Production      - lower crust (A2)  = 0.25e-6 W/m^3;
+#   Heat Production      - mantle (A3)       = 0.00e-6 W/m^3;
+#   Thermal Conductivity - all layers        = 2.5 (W/(m K));
+# To satisfy these constraints, the following values are required:
+#   Surface Temperature  - lower crust (ts2) = 633 K
+#                        - mantle (ts3)      = 893 K
+#   Surface Heat Flow    - lower crust (qs2) = 0.035 W/m^2;
+#                        - mantle      (qs3) = 0.030 W/m^2;
+# Note: The continental geotherm initial temperature model
+#       plugin can be used to compute an identical geotherm
+#       for the lithosphere. An example of how to use this
+#       plugin is illustrated in the test for this cookbook
+#       (tests/continental_extension.prm).
+subsection Initial temperature model
+  set Model name = function
+
+  subsection Function
+    set Variable names = x,y
+    set Function constants = h=100e3, ts1=273, ts2=633, ts3=893, \
+                             A1=1.e-6, A2=0.25e-6, A3=0.0, \
+                             k1=2.5, k2=2.5, k3=2.5, \
+                             qs1=0.055, qs2=0.035, qs3=0.030
+    set Function expression = if( (h-y)<=20.e3, \
+                                  ts1 + (qs1/k1)*(h-y) - (A1*(h-y)*(h-y))/(2.0*k1), \
+                                  if( (h-y)>20.e3 && (h-y)<=40.e3, \
+                                      ts2 + (qs2/k2)*(h-y-20.e3) - (A2*(h-y-20.e3)*(h-y-20.e3))/(2.0*k2), \
+                                      ts3 + (qs3/k3)*(h-y-40.e3) - (A3*(h-y-40.e3)*(h-y-40.e3))/(2.0*k3) ) );
+  end
+end
+
+# Constant internal heat production values (W/m^3) for background material
+# and compositional fields.
+subsection Heating model
+  set List of model names = compositional heating
+
+  subsection Compositional heating
+    set Use compositional field for heat production averaging = 1, 0, 0, 1, 1, 1
+    set Compositional heating values = 0.0, 0.0, 0.0, 1.0e-6, 0.25e-6, 0.
+  end
+end
+
+# Material model
+# Rheology: Non-linear viscous flow and Drucker Prager Plasticity
+# Values for most rheological parameters are specified for a background material and
+# each compositional field.  Values for viscous deformation are based on dislocation
+# creep flow-laws, with distinct values for the upper crust (wet quartzite), lower
+# crust (wet anorthite) and mantle (dry olivine).  Table 1 of Naliboff and Buiter (2015),
+# Earth Planet. Sci. Lett., v.421, p. 58-67 contains values for each of these flow laws.
+subsection Material model
+  set Model name = visco plastic
+
+  subsection Visco Plastic
+    # Reference temperature and viscosity
+    set Reference temperature = 273
+
+    # The minimum strain-rate helps limit large viscosities values that arise
+    # as the strain-rate approaches zero.
+    # The reference strain-rate is used on the first non-linear iteration
+    # of the first time step when the velocity has not been determined yet.
+    set Minimum strain rate = 1.e-20
+    set Reference strain rate = 1.e-16
+
+    # Limit the viscosity with minimum and maximum values
+    set Minimum viscosity = 1e18
+    set Maximum viscosity = 1e26
+
+    # Thermal diffusivity is adjusted to match thermal conductivities
+    # assumed in assigning the initial geotherm
+    set Define thermal conductivities = true
+    set Thermal conductivities        = 2.5
+    set Heat capacities               = 750.
+
+    # Density values of 1 are assigned to "strain" fields, which are not taken into
+    # account when computing material properties.
+    set Densities                     = 3300, 1.0, 1.0, 2700,  2900, 3300
+    set Thermal expansivities         = 2e-5
+
+    # Harmonic viscosity averaging
+    set Viscosity averaging scheme = harmonic
+
+    # Choose to have the viscosity (pre-yield) follow a dislocation
+    # diffusion or composite flow law.  Here, dislocation is selected
+    # so no need to specify diffusion creep parameters below, which are
+    # only used if "diffusion" or "composite" option is selected.
+    set Viscous flow law = dislocation
+
+    # Dislocation creep parameters for
+    # 1. Background material/mantle (dry olivine)
+    #    Hirth & Kohlstedt (2004),  Geophys. Monogr. Am. Geophys. Soc., v.138, p.83-105.
+    #    "Rheology of the upper mantle and the mantle wedge:a view from the experimentalists"
+    # 2. Upper crust (wet quartzite)
+    #    Rutter & Brodie (2004), J. Struct. Geol., v.26, p.2011-2023.
+    #    "Experimental grain size-sensitive flow of hot-pressed Brazilian quartz aggregates"
+    # 3. Lower crust and weak seed (wet anorthite)
+    #    Rybacki et al. (2006), J. Geophys. Res., v.111(B3).
+    #    "Influence of water fugacity and activation volume on the flow properties of fine-grained
+    #    anorthite aggregates"
+    # Note that the viscous pre-factors below are scaled to plane strain from unixial strain experiments.
+    # For ease of identification, fields tracking strain are assigned prefactors of 1e-50
+    set Prefactors for dislocation creep          = 6.52e-16, 1.00e-50, 1.00e-50, 8.57e-28, 7.13e-18, 6.52e-16
+    set Stress exponents for dislocation creep    =      3.5,      1.0,      1.0,      4.0,      3.0,      3.5
+    set Activation energies for dislocation creep =   530.e3,      0.0,      0.0,   223.e3,   345.e3,   530.e3
+    set Activation volumes for dislocation creep  =   18.e-6,      0.0,      0.0,      0.0,      0.0,   18.e-6
+
+    # Plasticity parameters
+    set Angles of internal friction = 30
+    set Cohesions                   = 20.e6
+
+    # The parameters below weaken the friction and cohesion by a
+    # a factor of 4 between plastic strain values of 0.5 and 1.5.
+    set Strain weakening mechanism                   = plastic weakening with plastic strain only
+    set Start plasticity strain weakening intervals  = 0.5
+    set End plasticity strain weakening intervals    = 1.5
+    set Cohesion strain weakening factors            = 0.25
+    set Friction strain weakening factors            = 0.25
+  end
+end
+
+# Gravity model
+subsection Gravity model
+  set Model name = vertical
+
+  subsection Vertical
+    set Magnitude = 9.81
+  end
+end
+
+# Post processing
+subsection Postprocess
+  set List of postprocessors = basic statistics, composition statistics, heat flux densities, heat flux statistics, mass flux statistics, matrix statistics, pressure statistics, temperature statistics, topography, velocity statistics, visualization
+
+  subsection Visualization
+    set List of output variables = density, heat flux map, named additional outputs, strain rate, viscosity
+    set Output format                 = vtu
+    set Time between graphical output = 100.e3
+    set Interpolate output            = true
+  end
+end

From c76090ad6359b4047ac3d874da00e104b13ce933 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Tue, 12 Dec 2023 12:32:24 +0100
Subject: [PATCH 03/38] Fix IC manager

---
 .../lithosphere_rift_IT.h                     |   9 +
 .../lithosphere_rift_IT_2.cc                  |  11 +-
 .../lithosphere_rift_topo.cc                  | 257 ++++++++++++++++++
 .../lithosphere_rift_topo.h                   | 159 +++++++++++
 4 files changed, 434 insertions(+), 2 deletions(-)
 create mode 100644 cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
 create mode 100644 cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
index 954ced16112..b9e9ba24bc9 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
@@ -24,6 +24,7 @@
 #define _aspect_initial_temperature_lithosphere_rift_h
 
 #include <aspect/initial_temperature/interface.h>
+#include <aspect/initial_composition/interface.h>
 #include <aspect/simulator_access.h>
 
 namespace aspect
@@ -144,6 +145,14 @@ namespace aspect
          */
         bool use_compensation_depth;
         double compensation_depth;
+
+        /**
+         * A shared pointer to the initial composition object
+         * that ensures that the current object can continue
+         * to access the initial composition object beyond the
+         * first time step.
+         */
+        std::shared_ptr<const aspect::InitialComposition::Manager<dim>> initial_composition_manager;
     };
   }
 }
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index 8df533ac492..e19185cc490 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -53,6 +53,13 @@ namespace aspect
       //AssertThrow((dynamic_cast<MaterialModel::ViscoPlasticStrain<dim> *> (const_cast<MaterialModel::Interface<dim> *>(&this->get_material_model()))) != 0,
       AssertThrow((dynamic_cast<MaterialModel::ViscoPlastic<dim> *> (const_cast<MaterialModel::Interface<dim> *>(&this->get_material_model()))) != 0,
                   ExcMessage("The lithosphere with rift initial temperature plugin requires the viscoplastic material model plugin."));
+
+      // The simulator only keeps the initial conditions around for
+      // the first time step. As a consequence, we have to save a
+      // shared pointer to that object ourselves the first time we get
+      // here.
+      if (initial_composition_manager == nullptr)
+        initial_composition_manager = this->get_initial_composition_manager_pointer();
     }
 
 
@@ -70,8 +77,8 @@ namespace aspect
       double distance_to_rift_axis = 1e23;
       Point<dim-1> surface_position;
       std::pair<double, unsigned int> distance_to_L_polygon;
-      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim> > >::const_iterator it = this->get_initial_composition_manager().get_active_initial_composition_conditions().begin();
-           it != this->get_initial_composition_manager().get_active_initial_composition_conditions().end();
+      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim> > >::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
+           it != initial_composition_manager->get_active_initial_composition_conditions().end();
            ++it)
         if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
           {
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
new file mode 100644
index 00000000000..2e08a66ff67
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -0,0 +1,257 @@
+/*
+  Copyright (C) 2016 by the authors of the ASPECT code.
+
+  This file is part of ASPECT.
+
+  ASPECT is free software; you can redistribute it and/or modify
+  it under the terms of the GNU General Public License as published by
+  the Free Software Foundation; either version 2, or (at your option)
+  any later version.
+
+  ASPECT is distributed in the hope that it will be useful,
+  but WITHOUT ANY WARRANTY; without even the implied warranty of
+  MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE.  See the
+  GNU General Public License for more details.
+
+  You should have received a copy of the GNU General Public License
+  along with ASPECT; see the file LICENSE.  If not see
+  <http://www.gnu.org/licenses/>.
+*/
+
+
+#include "lithosphere_rift_topo.h"
+#include "lithosphere_rift_IC.h"
+#include <aspect/geometry_model/box.h>
+#include <aspect/gravity_model/interface.h>
+#include <aspect/utilities.h>
+#include <boost/lexical_cast.hpp>
+
+namespace aspect
+{
+  namespace InitialTopographyModel
+  {
+    template <int dim>
+    void
+    LithosphereRift<dim>::
+    initialize ()
+    {
+      // Compute the maximum topography amplitude based on isostasy.
+      // Assume the reference density is representative for each layer (despite temperature dependence)
+
+      // For now, we assume a 3-layer system with an upper crust, lower crust and lithospheric mantle
+      const unsigned int id_upper = this->introspection().compositional_index_for_name("upper");
+      const unsigned int id_lower = this->introspection().compositional_index_for_name("lower");
+      const unsigned int id_mantle_L = this->introspection().compositional_index_for_name("mantle_L");
+
+      densities.push_back(temp_densities[0]);
+      densities.push_back(temp_densities[id_upper+1]);
+      densities.push_back(temp_densities[id_lower+1]);
+      densities.push_back(temp_densities[id_mantle_L+1]);
+
+      // The reference column
+      ref_rgh = 0;
+      // Assume constant gravity magnitude, so ignore
+      for (unsigned int l=0; l<3; ++l)
+        ref_rgh += densities[l+1] * thicknesses[l];
+
+      // The total lithosphere thickness
+      const double sum_thicknesses = std::accumulate(thicknesses.begin(), thicknesses.end(),0);
+
+      // Make sure the compensation depth is in the sublithospheric mantle
+      compensation_depth = 2. * sum_thicknesses + 1e3;
+
+      // The column at the rift center
+      double rift_rgh = 0;
+      rift_thicknesses = thicknesses;
+      for (unsigned int l=0; l<rift_thicknesses.size(); ++l)
+        rift_thicknesses[l] *= (1.-A[l]);
+
+      for (unsigned int l=0; l<3; ++l)
+        rift_rgh += densities[l+1] * rift_thicknesses[l];
+
+      // The total lithosphere thickness at the rift
+      const double sum_rift_thicknesses = std::accumulate(rift_thicknesses.begin(), rift_thicknesses.end(),0);
+
+      // The column at the polygon center
+      const unsigned int n_polygons = polygon_thicknesses.size();
+      std::vector<double> polygon_rgh(n_polygons);
+      std::vector<double> sum_polygon_thicknesses(n_polygons);
+      for (unsigned int i_polygons=0; i_polygons<n_polygons; ++i_polygons)
+        {
+          for (unsigned int l=0; l<3; ++l)
+            {
+              polygon_rgh[i_polygons] += densities[l+1] * polygon_thicknesses[i_polygons][l];
+            }
+          // The total lithosphere thickness
+          sum_polygon_thicknesses[i_polygons] = std::accumulate(polygon_thicknesses[i_polygons].begin(), polygon_thicknesses[i_polygons].end(),0);
+          polygon_rgh[i_polygons] += (compensation_depth - sum_polygon_thicknesses[i_polygons]) * densities[0];
+        }
+
+      // Add sublithospheric mantle part to the columns
+      ref_rgh += (compensation_depth - sum_thicknesses) * densities[0];
+      rift_rgh += (compensation_depth - sum_rift_thicknesses) * densities[0];
+
+      // Compute the maximum topography based on mass surplus/deficit
+      topo_rift_amplitude = (ref_rgh-rift_rgh) / densities[0];
+      for (unsigned int i_polygons=0; i_polygons<n_polygons; ++i_polygons)
+        topo_polygon_amplitude = std::max((ref_rgh-polygon_rgh[i_polygons]) / densities[0],topo_polygon_amplitude);
+
+      // TODO: probably there are combinations of rift and polygon topography
+      // that result in a higher topography
+      maximum_topography = std::max(topo_rift_amplitude, topo_polygon_amplitude);
+
+      this->get_pcout() << "   Maximum initial topography of rift: " << topo_rift_amplitude << " m" << std::endl;
+      this->get_pcout() << "   Maximum initial topography of polygon: " << topo_polygon_amplitude << " m" << std::endl;
+
+      // The simulator only keeps the initial conditions around for
+      // the first time step. As a consequence, we have to save a
+      // shared pointer to that object ourselves the first time we get
+      // here.
+      if (initial_composition_manager == nullptr)
+        initial_composition_manager = this->get_initial_composition_manager_pointer();
+    }
+
+
+    template <int dim>
+    double
+    LithosphereRift<dim>::
+    value (const Point<dim-1> &position) const
+    {
+      // Check that the required initial composition model is used
+      // We have to do it here instead of in initialize() because
+      // the names are not available upon initialization of the
+      // initial topography model yet.
+      const std::vector<std::string> active_initial_composition_models = initial_composition_manager->get_active_initial_composition_names();
+      AssertThrow(std::find(active_initial_composition_models.begin(),active_initial_composition_models.end(), "lithosphere with rift") != active_initial_composition_models.end(),
+                  ExcMessage("The lithosphere with rift initial mesh refinement plugin requires the lithosphere with rift initial composition plugin."));
+
+      // When cartesian, position contains x(,y); when spherical, position contains lon(,lat) (in degrees);
+      // Turn into a Point<dim-1>
+      Point<dim-1> surface_position;
+      for (unsigned int d=0; d<dim-1; ++d)
+        surface_position[d] = position[d];
+
+      // Get the distance to the line segments along a path parallel to the surface
+      double distance_to_rift_axis = 1e23;
+      std::pair<double,unsigned int> distance_to_L_polygon;
+      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim> > >::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
+           it != initial_composition_manager->get_active_initial_composition_conditions().end();
+           ++it)
+        if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
+          {
+            distance_to_rift_axis = ic->distance_to_rift(surface_position);
+            distance_to_L_polygon = ic->distance_to_polygon(surface_position);
+          }
+
+      // Compute the topography based on distance to the rift and distance to the polygon
+      std::vector<double> local_thicknesses(3);
+      local_thicknesses[0] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][0]
+                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[0])
+                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
+                               (1.0 - A[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      local_thicknesses[1] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
+                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
+                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
+                               (1.0 - A[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      local_thicknesses[2] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
+                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
+                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
+                               (1.0 - A[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+
+      // The local lithospheric column
+      double local_rgh = 0;
+      for (unsigned int l=0; l<3; ++l)
+        local_rgh += densities[l+1] * local_thicknesses[l];
+      // The total local lithosphere thickness
+      const double sum_local_thicknesses = std::accumulate(local_thicknesses.begin(), local_thicknesses.end(),0);
+      local_rgh += (compensation_depth - sum_local_thicknesses) * densities[0];
+
+      return (ref_rgh - local_rgh) / densities[0];
+    }
+
+
+    template <int dim>
+    double
+    LithosphereRift<dim>::
+    max_topography () const
+    {
+      return maximum_topography;
+    }
+
+
+    template <int dim>
+    void
+    LithosphereRift<dim>::
+    declare_parameters (ParameterHandler &)
+    {
+    }
+
+
+
+    template <int dim>
+    void
+    LithosphereRift<dim>::parse_parameters (ParameterHandler &prm)
+    {
+      unsigned int n_fields;
+      prm.enter_subsection ("Compositional fields");
+      {
+        n_fields = prm.get_integer ("Number of fields");
+      }
+      prm.leave_subsection();
+      prm.enter_subsection ("Initial composition model");
+      {
+        prm.enter_subsection("Lithosphere with rift");
+        {
+          sigma_rift           = prm.get_double ("Standard deviation of Gaussian rift geometry");
+          sigma_polygon        = prm.get_double ("Half width of polygon smoothing");
+          blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
+          A                    = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
+                                                                         3,
+                                                                         "Amplitude of Gaussian rift geometry");
+          thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
+                                                                3,
+                                                                "Layer thicknesses");
+          // Split the string into the separate polygons
+          const std::vector<std::string> temp_thicknesses = Utilities::split_string_list(prm.get("Lithospheric polygon layer thicknesses"),';');
+          const unsigned int n_polygons = temp_thicknesses.size();
+          polygon_thicknesses.resize(n_polygons);
+          for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
+            {
+              polygon_thicknesses[i_polygons] = Utilities::string_to_double(Utilities::split_string_list(temp_thicknesses[i_polygons],','));
+              AssertThrow(polygon_thicknesses[i_polygons].size()==3, ExcMessage ("The number of layer thicknesses should be equal to 3."));
+            }
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+
+
+      prm.enter_subsection("Material model");
+      {
+        prm.enter_subsection("Visco Plastic");
+        {
+          // The material model viscoplastic prefixes an entry for the background material
+          temp_densities = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Densities"))),
+                                                                   n_fields+1,
+                                                                   "Densities");
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+    }
+  }
+}
+
+// explicit instantiations
+namespace aspect
+{
+  namespace InitialTopographyModel
+  {
+    ASPECT_REGISTER_INITIAL_TOPOGRAPHY_MODEL(LithosphereRift,
+                                             "lithosphere with rift",
+                                             "An initial topography model that defines the initial topography "
+                                             "based on isostasy. It takes into account lithospheric thickness "
+                                             "variations as specified in the InitialComposition model lithosphere "
+                                             "with rift' as should only be used in conjunction with this model. ")
+  }
+}
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
new file mode 100644
index 00000000000..ae3931eb0c0
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
@@ -0,0 +1,159 @@
+/*
+  Copyright (C) 2016 by the authors of the ASPECT code.
+
+  This file is part of ASPECT.
+
+  ASPECT is free software; you can redistribute it and/or modify
+  it under the terms of the GNU General Public License as published by
+  the Free Software Foundation; either version 2, or (at your option)
+  any later version.
+
+  ASPECT is distributed in the hope that it will be useful,
+  but WITHOUT ANY WARRANTY; without even the implied warranty of
+  MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE.  See the
+  GNU General Public License for more details.
+
+  You should have received a copy of the GNU General Public License
+  along with ASPECT; see the file LICENSE.  If not see
+  <http://www.gnu.org/licenses/>.
+*/
+
+
+#ifndef _aspect_geometry_model__initial_topography_lithosphere_rift_h
+#define _aspect_geometry_model__initial_topography_lithosphere_rift_h
+
+#include <aspect/geometry_model/initial_topography_model/interface.h>
+#include <aspect/initial_composition/interface.h>
+
+namespace aspect
+{
+  namespace InitialTopographyModel
+  {
+    using namespace dealii;
+
+    /**
+     * A class that describes an initial topography for the geometry model,
+     * by defining a set of polylines on the surface from the prm file. It
+     * sets the elevation in each Polyline to a constant value.
+     */
+    template <int dim>
+    class LithosphereRift : public Interface<dim>,
+      public SimulatorAccess<dim>
+    {
+      public:
+        /**
+         * Initialization function. This function is called once at the
+         * beginning of the program. Checks preconditions.
+         */
+        void
+        initialize ();
+
+        /**
+         * Return the value of the topography for a point.
+         */
+        virtual
+        double value (const Point<dim-1> &p) const;
+
+        /**
+         * Return the maximum value of the elevation.
+         */
+        virtual
+        double max_topography () const;
+
+        /**
+         * Declare the parameters this class takes through input files.
+         */
+        static
+        void
+        declare_parameters (ParameterHandler &prm);
+
+        /**
+         * Read the parameters this class declares from the parameter file.
+         */
+        virtual
+        void
+        parse_parameters (ParameterHandler &prm);
+
+      private:
+        /**
+         * The standard deviation of the Gaussian amplitude of the lithospheric thicknesses
+         * with distance from the rift axis.
+         */
+        double sigma_rift;
+
+        /**
+         * The half width of the hyperbolic tangent used to smooth the transitions
+         * between reference and polygon lithospheric thicknesses.
+         */
+        double sigma_polygon;
+
+        /**
+         * The maximum amplitude of the Gaussian distribution of the lithospheric thicknesses
+         * with distance from the rift axis. It should have values between -1 and 1, where positive
+         * numbers represent a reduction in thickness and negative numbers an increase.
+         */
+        std::vector<double> A;
+
+        /**
+         * The maximum amplitude of the Gaussian distribution of the topography around the rift.
+         */
+        double topo_rift_amplitude;
+
+        /**
+         * The reference lithospheric column used in computing the topography based on isostasy
+         * and the thickness of this column.
+         */
+        double ref_rgh;
+        double compensation_depth;
+
+        /**
+         * Wheter or not to take the polygon thicknesses as dominant, or to smooth them
+         * gradually into rift areas.
+         */
+        bool blend_rift_and_polygon;
+
+
+        /**
+         * The maximum amplitude of the topography of the polygon area.
+         */
+        double topo_polygon_amplitude;
+
+        /**
+         * Vector for field densities.
+         */
+        std::vector<double> densities;
+        std::vector<double> temp_densities;
+
+        /**
+         * Vector for the reference field thicknesses away from the rift.
+         */
+        std::vector<double> thicknesses;
+
+        /**
+         * Vector for the rift  thicknesses at the center.
+         */
+        std::vector<double> rift_thicknesses;
+
+        /**
+         * Vector for the polygon thicknesses at the center.
+         */
+        std::vector<std::vector<double> > polygon_thicknesses;
+
+        /**
+         * The maximum topography in this model
+         */
+        double maximum_topography;
+
+        /**
+         * A shared pointer to the initial composition object
+         * that ensures that the current object can continue
+         * to access the initial composition object beyond the
+         * first time step.
+         */
+        std::shared_ptr<const aspect::InitialComposition::Manager<dim>> initial_composition_manager;
+    };
+  }
+}
+
+
+#endif

From e0d87bdc411cacb4c8b63208131b9e8483e0906c Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Tue, 12 Dec 2023 17:49:43 +0100
Subject: [PATCH 04/38] Set plastic strain grid to 10 km extra

---
 .../rift_box_initial_plastic_strain.h                           | 2 +-
 1 file changed, 1 insertion(+), 1 deletion(-)

diff --git a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
index 6003e0c26ab..099c5274201 100644
--- a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
+++ b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
@@ -153,7 +153,7 @@ namespace aspect
          * The height we add to vertical domain extent
          * to deal with any initial topography.
          */
-        const double maximum_initial_topography = 5000.;
+        const double maximum_initial_topography = 10000.;
     };
   }
 }

From 1d40c4ff89b95a9fb5e20829c0cc62e4d9b3ea9c Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Wed, 13 Dec 2023 15:37:00 +0100
Subject: [PATCH 05/38] Move get_pointer to where it exists

---
 .../lithosphere_rift_topo.cc                         | 12 ++++++------
 1 file changed, 6 insertions(+), 6 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
index 2e08a66ff67..d5f3d67fb28 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -103,12 +103,6 @@ namespace aspect
       this->get_pcout() << "   Maximum initial topography of rift: " << topo_rift_amplitude << " m" << std::endl;
       this->get_pcout() << "   Maximum initial topography of polygon: " << topo_polygon_amplitude << " m" << std::endl;
 
-      // The simulator only keeps the initial conditions around for
-      // the first time step. As a consequence, we have to save a
-      // shared pointer to that object ourselves the first time we get
-      // here.
-      if (initial_composition_manager == nullptr)
-        initial_composition_manager = this->get_initial_composition_manager_pointer();
     }
 
 
@@ -117,6 +111,12 @@ namespace aspect
     LithosphereRift<dim>::
     value (const Point<dim-1> &position) const
     {
+      // The simulator only keeps the initial conditions around for
+      // the first time step. As a consequence, we have to save a
+      // shared pointer to that object ourselves the first time we get
+      // here.
+      if (initial_composition_manager == nullptr)
+        const_cast<std::shared_ptr<const aspect::InitialComposition::Manager<dim>>&>(initial_composition_manager) = this->get_initial_composition_manager_pointer();
       // Check that the required initial composition model is used
       // We have to do it here instead of in initialize() because
       // the names are not available upon initialization of the

From e96875fe7199e1fe347b0ec26016aeebb627898a Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 14 Dec 2023 11:19:43 +0100
Subject: [PATCH 06/38] Update prm

---
 .../initial_conditions_continental_rift.prm   | 107 ++++++++++++++----
 1 file changed, 83 insertions(+), 24 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
index 40cc2cfeca6..2859f28ae40 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
@@ -22,7 +22,7 @@ set End time                               = 5e6
 set Use years in output instead of seconds = true
 set Nonlinear solver scheme                = single Advection, iterated defect correction Stokes
 set Nonlinear solver tolerance             = 1e-4
-set Max nonlinear iterations               = 100
+set Max nonlinear iterations               = 2
 set CFL number                             = 0.5
 set Maximum time step                      = 20e3
 set Output directory                       = output-continental_extension
@@ -53,7 +53,7 @@ end
 # undergoing brittle deformation are in the high-resolution
 # region.
 subsection Mesh refinement
-  set Initial adaptive refinement        = 1
+  set Initial adaptive refinement        = 0
   set Initial global refinement          = 3
   set Time steps between mesh refinement = 0
   set Strategy = minimum refinement function
@@ -124,7 +124,7 @@ end
 # 5. The mantle lithosphere
 subsection Compositional fields
   set Number of fields = 5
-  set Names of fields = noninitial_plastic_strain, plastic_strain, upper_crust, lower_crust, mantle_lithosphere
+  set Names of fields = noninitial_plastic_strain, plastic_strain, upper, lower, mantle_L
 end
 
 # Initial values of different compositional fields
@@ -134,35 +134,65 @@ end
 # to 0 and the initial plastic strain is randomized between
 # 0.5 and 1.5.
 subsection Initial composition model
-  set List of model names = function, rift box initial plastic strain #lithosphere with rift
-#  subsection Lithosphere with rift
-#    set Blend polygons and rifts                       = true
-#    set Standard deviation of Gaussian rift geometry   = 60e3
-#    set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
+  set List of model names = lithosphere with rift, rift box initial plastic strain, function
+
+  subsection Lithosphere with rift
+    set Blend polygons and rifts                       = true
+    set Standard deviation of Gaussian rift geometry   = 60e3
+    set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
     # LAB at 110 km
-#    set Rift axis line segments                        = 350e3  
-#    set Layer thicknesses                              = 20e3, 15e3, 85e3
+    set Rift axis line segments                        = 350e3  
+    set Layer thicknesses                              = 20e3, 15e3, 85e3
    
     # Polygon LAB at 200 km
-#    set Lithospheric polygon layer thicknesses         = 23e3, 20e3 , 157.e3
-#    set Lithospheric polygons                          = 450e3 > 3000e3
-#    set Half width of polygon smoothing                = 10e3 
-#  end
-
+    set Lithospheric polygon layer thicknesses         = 23e3, 20e3 , 157.e3
+    set Lithospheric polygons                          = 450e3 > 3000e3
+    set Half width of polygon smoothing                = 10e3 
+  end
+  
+  # Inherited noise 
+  subsection Rift box initial plastic strain
+    set Standard deviation of Gaussian noise amplitude distribution 	= 200e3    
+    set Maximum amplitude of Gaussian noise amplitude distribution      = 0.250000
+    set Random number generator seed                                    = 2.000000
+    set Depth around which Gaussian noise is smoothed out               = 50e3      
+    set Halfwidth with which Gaussian noise is smoothed out in depth    = 10e3         
+    #set Grid intervals for noise X or radius                            = 2240
+    # Add 16 intervals for the additional 5 km that is added to the grid
+    # to account for initial topography
+    #set Grid intervals for noise Y or longitude                         = 976 #960
+    set Rift axis line segments                                         = 350e3
+  end
+  
   subsection Function
-    set Variable names      = x,y
-    set Function expression = 0; \
-                              if(x>50.e3 && x<150.e3 && y>50.e3, 0.5 + rand_seed(1), 0); \
-                              if(y>=80.e3, 1, 0); \
-                              if(y<80.e3 && y>=60.e3, 1, 0); \
-                              if(y<60.e3, 1, 0);
+    set Variable names = x,y
+    set Function expression           = 0; \
+                                        0; \
+                                        0; \
+					0; \
+					0
   end
+#  subsection Function
+#    set Variable names      = x,y
+#    set Function expression = 0; \
+#                              if(x>50.e3 && x<150.e3 && y>50.e3, 0.5 + rand_seed(1), 0); \
+#                              if(y>=80.e3, 1, 0); \
+#                              if(y<80.e3 && y>=60.e3, 1, 0); \
+#                              if(y<60.e3, 1, 0);
+#  end
 end
 
 # Composition: fixed on bottom (inflow boundary), free on sides and top
 subsection Boundary composition model
   set Fixed composition boundary indicators = bottom
-  set List of model names = initial composition
+  set List of model names = function
+  subsection Function
+    set Function expression           = 0; \
+                                        0; \
+                                        0; \
+					0; \
+					0
+  end
 end
 
 # Temperature boundary conditions
@@ -202,7 +232,36 @@ end
 #       plugin is illustrated in the test for this cookbook
 #       (tests/continental_extension.prm).
 subsection Initial temperature model
-  set Model name = function
+  set List of model names = adiabatic, lithosphere with rift
+  set List of model operators = add, replace if valid
+  subsection Lithosphere with rift
+    set LAB isotherm temperature = 1623.
+    set Surface temperature = 293.
+    # Whether or not to prescribe the LAB depth up to a
+    # certain depth (in area below LAB)
+    # or use adiabat everywhere
+    set Use temperature compensation depth = true
+    set Temperature compensation depth = 200e3
+  end
+  subsection Adiabatic
+    # A reference profile of the compositional fields
+    # where x represents depth
+    subsection Function
+    #  plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio_marine_continental_sediment, silt_fraction
+       set Function expression           = 0; \
+                                           0; \
+                                           0; \
+                                           0; \
+					   0; \
+                                           if(x<23e3,1,0); \
+                                           if(x>=23e3&x<43e3,1,0); \
+                                           if(x>=43e3&x<200e3,1,0); \
+                                           0; \
+                                           0
+    end
+    set Age top boundary layer        = 0
+    set Age bottom boundary layer     = 0
+  end
 
   subsection Function
     set Variable names = x,y
@@ -317,7 +376,7 @@ end
 
 # Post processing
 subsection Postprocess
-  set List of postprocessors = basic statistics, composition statistics, heat flux densities, heat flux statistics, mass flux statistics, matrix statistics, pressure statistics, temperature statistics, topography, velocity statistics, visualization
+  set List of postprocessors = composition statistics, heat flux densities, heat flux statistics, mass flux statistics, pressure statistics, temperature statistics, topography, velocity statistics, visualization
 
   subsection Visualization
     set List of output variables = density, heat flux map, named additional outputs, strain rate, viscosity

From 73e9eeb4690bb48017ad2cd89aa3c649163d63e6 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 30 Sep 2022 14:02:04 +0200
Subject: [PATCH 07/38] Store pointer and update read-in density initial
 temperature

---
 .../lithosphere_rift_IT.h                     | 10 +++++
 .../lithosphere_rift_IT_2.cc                  | 39 +++++++++++++++----
 2 files changed, 41 insertions(+), 8 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
index b9e9ba24bc9..24cc4c3fff4 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
@@ -153,6 +153,16 @@ namespace aspect
          * first time step.
          */
         std::shared_ptr<const aspect::InitialComposition::Manager<dim>> initial_composition_manager;
+
+        /**
+         * Vector containing the number of phases for each composition.
+         */
+        std::unique_ptr<std::vector<unsigned int>> n_phases_for_each_composition;
+
+        /**
+         * Vector containing the names of the compositional fields.
+         */
+        std::vector<std::string> list_of_composition_names;
     };
   }
 }
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index e19185cc490..9c6c084f5bc 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -77,7 +77,7 @@ namespace aspect
       double distance_to_rift_axis = 1e23;
       Point<dim-1> surface_position;
       std::pair<double, unsigned int> distance_to_L_polygon;
-      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim> > >::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
+      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim>>>::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
            it != initial_composition_manager->get_active_initial_composition_conditions().end();
            ++it)
         if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
@@ -260,14 +260,16 @@ namespace aspect
       }
       prm.leave_subsection();
 
+      prm.enter_subsection ("Compositional fields");
+      {
+        list_of_composition_names = Utilities::split_string_list (prm.get("Names of fields"));
+      }
+      prm.leave_subsection();
+
       prm.enter_subsection("Material model");
       {
         prm.enter_subsection("Visco Plastic");
         {
-          // The material model viscoplastic prefixes an entry for the background material
-          const std::vector<double> temp_densities = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Densities"))),
-                                                     n_fields+1,
-                                                     "Densities");
           const std::vector<double> temp_thermal_diffusivities = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Thermal diffusivities"))),
                                                                  n_fields+1,
                                                                  "Thermal diffusivities");
@@ -275,9 +277,30 @@ namespace aspect
                                                            n_fields+1,
                                                            "Heat capacities");
 
-          densities.push_back(temp_densities[id_upper+1]);
-          densities.push_back(temp_densities[id_lower+1]);
-          densities.push_back(temp_densities[id_mantle_L+1]);
+          n_phases_for_each_composition = std::make_unique<std::vector<unsigned int>>();
+          const std::vector<double> temp_densities = Utilities::parse_map_to_double_array (prm.get("Densities"),
+                                                     list_of_composition_names,
+                                                     /*has_background_field=*/true,
+                                                     "Densities",
+                                                     true,
+                                                     n_phases_for_each_composition);
+
+          // Assemble a list of phase densities for each composition.
+          // Add 1 for background material.
+          std::vector<std::vector<double>> densities_per_composition(this->n_compositional_fields()+1);
+          unsigned int counter = 0;
+          for (unsigned int i = 0; i < (*n_phases_for_each_composition).size(); ++i)
+            {
+              for (unsigned int j = 0; j < (*n_phases_for_each_composition)[i]; ++j)
+                {
+                  densities_per_composition[i].push_back(temp_densities[counter]);
+                  ++counter;
+                }
+            }
+
+          densities.push_back(densities_per_composition[id_upper+1][0]);
+          densities.push_back(densities_per_composition[id_lower+1][0]);
+          densities.push_back(densities_per_composition[id_mantle_L+1][0]);
 
           // Thermal diffusivity kappa = k/(rho*cp), so thermal conducitivity k = kappa*rho*cp
           conductivities.push_back(temp_thermal_diffusivities[id_upper+1] * densities[0] * temp_heat_capacities[id_upper+1]);

From fd37a9b27811c94c340ddf18afffdba418e57513 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 30 Sep 2022 11:58:56 +0200
Subject: [PATCH 08/38] Update read-in densities initial topography

---
 .../lithosphere_rift_topo.cc                  | 41 +++++++++++++++----
 .../lithosphere_rift_topo.h                   | 10 +++++
 2 files changed, 43 insertions(+), 8 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
index d5f3d67fb28..8a6cb1bac45 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -43,10 +43,27 @@ namespace aspect
       const unsigned int id_lower = this->introspection().compositional_index_for_name("lower");
       const unsigned int id_mantle_L = this->introspection().compositional_index_for_name("mantle_L");
 
-      densities.push_back(temp_densities[0]);
-      densities.push_back(temp_densities[id_upper+1]);
-      densities.push_back(temp_densities[id_lower+1]);
-      densities.push_back(temp_densities[id_mantle_L+1]);
+      // Assemble a list of phase densities for each composition.
+      // Add 1 for background material.
+      std::vector<std::vector<double>> densities_per_composition(this->n_compositional_fields()+1);
+      unsigned int counter = 0;
+      for (unsigned int i = 0; i < (*n_phases_for_each_composition).size(); ++i)
+        {
+          for (unsigned int j = 0; j < (*n_phases_for_each_composition)[i]; ++j)
+            {
+              densities_per_composition[i].push_back(temp_densities[counter]);
+              ++counter;
+            }
+        }
+
+      // Get the relevant densities for the lithosphere.
+      densities.push_back(densities_per_composition[0][0]);
+      densities.push_back(densities_per_composition[id_upper+1][0]);
+      densities.push_back(densities_per_composition[id_lower+1][0]);
+      densities.push_back(densities_per_composition[id_mantle_L+1][0]);
+      std::cout << "Assembling final densities: " << densities_per_composition[0][0] << ", ";
+      std::cout << densities_per_composition[id_upper+1][0] << ", " << densities_per_composition[id_lower+1][0];
+      std::cout  << ", " <<  densities_per_composition[id_mantle_L+1][0] <<  std::endl;
 
       // The reference column
       ref_rgh = 0;
@@ -225,15 +242,23 @@ namespace aspect
       }
       prm.leave_subsection();
 
+      prm.enter_subsection ("Compositional fields");
+      {
+        list_of_composition_names = Utilities::split_string_list (prm.get("Names of fields"));
+      }
+      prm.leave_subsection();
 
       prm.enter_subsection("Material model");
       {
         prm.enter_subsection("Visco Plastic");
         {
-          // The material model viscoplastic prefixes an entry for the background material
-          temp_densities = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Densities"))),
-                                                                   n_fields+1,
-                                                                   "Densities");
+          n_phases_for_each_composition = std::make_unique<std::vector<unsigned int>>();
+          temp_densities = Utilities::parse_map_to_double_array (prm.get("Densities"),
+                                                                 list_of_composition_names,
+                                                                 /*has_background_field=*/true,
+                                                                 "Densities",
+                                                                 true,
+                                                                 n_phases_for_each_composition);
         }
         prm.leave_subsection();
       }
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
index ae3931eb0c0..d6f6411daae 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
@@ -151,6 +151,16 @@ namespace aspect
          * first time step.
          */
         std::shared_ptr<const aspect::InitialComposition::Manager<dim>> initial_composition_manager;
+
+        /**
+         * Vector containing the number of phases for each composition.
+         */
+        std::unique_ptr<std::vector<unsigned int>> n_phases_for_each_composition;
+
+        /**
+         * Vector containing the names of the compositional fields.
+         */
+        std::vector<std::string> list_of_composition_names;
     };
   }
 }

From 785f7d1f0c42ca698bc1d1acf7d4e04af0687ae2 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Sun, 17 Dec 2023 18:12:19 +0100
Subject: [PATCH 09/38] Remove unused parameter

---
 .../lithosphere_rift_topo.cc                                | 6 ------
 1 file changed, 6 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
index 8a6cb1bac45..50556895053 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -209,12 +209,6 @@ namespace aspect
     void
     LithosphereRift<dim>::parse_parameters (ParameterHandler &prm)
     {
-      unsigned int n_fields;
-      prm.enter_subsection ("Compositional fields");
-      {
-        n_fields = prm.get_integer ("Number of fields");
-      }
-      prm.leave_subsection();
       prm.enter_subsection ("Initial composition model");
       {
         prm.enter_subsection("Lithosphere with rift");

From 1236592075f78a8bb8171f9b53b385ec6e9165e4 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Sun, 17 Dec 2023 18:12:38 +0100
Subject: [PATCH 10/38] Fix compiler warnings

---
 .../rift_box_initial_plastic_strain.cc                    | 8 +++++---
 .../rift_box_initial_plastic_strain.h                     | 2 +-
 2 files changed, 6 insertions(+), 4 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
index e93162f67fa..54b46f0db46 100644
--- a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
+++ b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
@@ -147,7 +147,7 @@ namespace aspect
         prm.enter_subsection("Rift box initial plastic strain");
         {
           prm.declare_entry ("Random number generator seed", "0",
-                             Patterns::Double (0),
+                             Patterns::Integer (0),
                              "The value of the seed used for the random number generator. "
                              "Units: none.");
           prm.declare_entry ("Standard deviation of Gaussian noise amplitude distribution", "20000",
@@ -229,8 +229,10 @@ namespace aspect
       prm.leave_subsection();
 
       // The grid intervals equal the number of mesh cells.
+      // refinement, repetitions and grid_intervals are integers,
+      // but pow returns a double, so convert to int.
       for (unsigned int d = 0; d < dim; ++d)
-        grid_intervals[d] = repetitions[d] * std::pow(2, refinement);
+        grid_intervals[d] = repetitions[d] * int(std::pow(2, refinement));
 
       // Both initial mesh deformation and initial topography models
       // can distort the initial mesh such that the vertical coordinate
@@ -254,7 +256,7 @@ namespace aspect
         prm.enter_subsection("Rift box initial plastic strain");
         sigma                = prm.get_double ("Standard deviation of Gaussian noise amplitude distribution");
         A                    = prm.get_double ("Maximum amplitude of Gaussian noise amplitude distribution");
-        seed                 = prm.get_double ("Random number generator seed");
+        seed                 = prm.get_integer ("Random number generator seed");
         strain_height        = origin[dim-1] + extents[dim-1] - prm.get_double ("Depth around which Gaussian noise is smoothed out");
         strain_halfwidth     = prm.get_double ("Halfwidth with which Gaussian noise is smoothed out in depth");
 
diff --git a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
index 099c5274201..8413f4ccb3d 100644
--- a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
+++ b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
@@ -93,7 +93,7 @@ namespace aspect
         /**
          * The value of the seed for the random number generator
          */
-        double seed;
+        unsigned int seed;
 
         /**
          * The maximum amplitude of the Gaussian amplitude of the noise.

From 532f8fbead070e1cdaae576e6f37734a7d5e3ad1 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Tue, 2 Jan 2024 19:35:01 +0100
Subject: [PATCH 11/38] Clean up

---
 .../lithosphere_rift_IC.cc                    | 203 +++++++++---------
 .../lithosphere_rift_IC.h                     |  49 +++--
 2 files changed, 130 insertions(+), 122 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
index 808a4349b49..0c32696912b 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
@@ -34,7 +34,7 @@ namespace aspect
     LithosphereRift<dim>::
     initialize ()
     {
-      // Check that the required initial composition model is used
+      // Check that the corresponding initial temperature model is used.
       const std::vector<std::string> active_initial_temperature_models = this->get_initial_temperature_manager().get_active_initial_temperature_names();
       AssertThrow(find(active_initial_temperature_models.begin(),active_initial_temperature_models.end(), "lithosphere with rift") != active_initial_temperature_models.end(),
                   ExcMessage("The lithosphere with rift initial composition plugin requires the lithosphere with rift initial temperature plugin."));
@@ -47,45 +47,48 @@ namespace aspect
                          const unsigned int compositional_index) const
     {
       // Retrieve the indices of the fields that represent the lithospheric layers.
-      // We assume a 3-layer system with an upper crust, lower crust and lithospheric mantle
+      // We assume a 3-layer system with an upper crust, lower crust and lithospheric mantle.
       const unsigned int id_upper = this->introspection().compositional_index_for_name("upper");
       const unsigned int id_lower = this->introspection().compositional_index_for_name("lower");
       const unsigned int id_mantle_L = this->introspection().compositional_index_for_name("mantle_L");
 
       // Determine coordinate system
-      const bool cartesian_geometry = dynamic_cast<const GeometryModel::Box<dim> *>(&this->get_geometry_model()) != NULL ? true : false;
+      const bool cartesian_geometry = Plugins::plugin_type_matches<const GeometryModel::Box<dim>> (this->get_geometry_model());
 
+      // Get the surface coordinates of the point under consideration
       const Point<dim-1> surface_point = surface_position(position, cartesian_geometry);
 
-      // Get the distance to the line segments along a path parallel to the surface
+      // Get the distance to the rift segments along a path parallel to the surface
       const double distance_to_rift_axis = distance_to_rift(surface_point);
 
-      // Get the signed distance to a polygon of different lithospheric thicknesses
+      // Get the signed distance to potential polygons of different lithospheric thicknesses
       const std::pair<double, unsigned int> distance_to_L_polygon = distance_to_polygon(surface_point);
 
       // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
       // (in this exact order) based on the distance from the rift axis.
-      const double local_upper_crust_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][0]
-                                                  +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[0])
-                                                 * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-      const double local_lower_crust_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
-                                                  +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
-                                                 * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-      const double local_mantle_lithosphere_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
-                                                         +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
-                                                        *  (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-
-//sb      std::cout << "Initial compo " << position[0] << " " << compositional_index << " " << local_upper_crust_thickness << " " << local_lower_crust_thickness << " " << local_mantle_lithosphere_thickness << std::endl;
-
-      // Compute depth
+      std::vector <double> local_thicknesses(3);
+      for (unsigned int i = 0; i<3; ++i)
+        local_thicknesses[i] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][i]
+                                +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[i])
+                               * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      //const double local_lower_crust_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
+      //                                            +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[1])
+      //                                           * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      //const double local_mantle_lithosphere_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
+      //                                                   +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[2])
+      //                                                  *  (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+
+      // Get depth with respect to the surface.
       const double depth = this->get_geometry_model().depth(position);
 
-      // Check which layer we're in and return value.
-      if (depth <= local_upper_crust_thickness && compositional_index == id_upper)
+      // Check which layer the current point lies in and return a value of 1 if the field corresponds to the layer.
+      if (depth <= local_thicknesses[0] && compositional_index == id_upper)
         return 1.;
-      else if (depth > local_upper_crust_thickness && depth <= local_upper_crust_thickness+local_lower_crust_thickness && compositional_index == id_lower)
+      else if (depth > local_thicknesses[0] && depth <= local_thicknesses[0] + local_thicknesses[1]
+               && compositional_index == id_lower)
         return 1.;
-      else if (depth > local_upper_crust_thickness+local_lower_crust_thickness && depth <= local_upper_crust_thickness+local_lower_crust_thickness+local_mantle_lithosphere_thickness && compositional_index == id_mantle_L)
+      else if (depth > local_thicknesses[0] + local_thicknesses[2] && depth <= local_thicknesses[0] + local_thicknesses[1] + local_thicknesses[2]
+               && compositional_index == id_mantle_L)
         return 1.;
       else
         return 0.;
@@ -101,9 +104,11 @@ namespace aspect
       double temp_distance = 0;
 
       // Loop over all line segments
-      for (unsigned int i_segments = 0; i_segments < point_list.size(); ++i_segments)
+      for (unsigned int i_segments = 0; i_segments < rift_point_list.size(); ++i_segments)
         {
-          temp_distance = (dim == 2) ? std::abs(surface_position[0]-point_list[i_segments][0][0]) : std::abs(Utilities::distance_to_line(point_list[i_segments], Point<2>(surface_position[0],surface_position[dim-2])));
+          // The Utilities function only works in 3d, so compute distance here in 2d.
+          temp_distance = (dim == 2) ? std::abs(surface_position[0]-rift_point_list[i_segments][0][0])
+                          : std::abs(Utilities::distance_to_line(rift_point_list[i_segments], Point<2>(surface_position[0],surface_position[dim-2])));
 
           // Get the minimum distance
           distance_to_rift_axis = std::min(distance_to_rift_axis, temp_distance);
@@ -124,10 +129,10 @@ namespace aspect
           for (unsigned int d=0; d<dim-1; ++d)
             surface_point[d]=position[d];
         }
-      // chunk (spherical) geometries
+      // chunk or spherical geometries
       else
         {
-          // spherical coordinates in radius [m], lon [rad], colat [rad] format
+          // Get spherical coordinates in radius [m], lon [rad], colat [rad] format
           const std::array<double,dim> spherical_point = Utilities::Coordinates::cartesian_to_spherical_coordinates(position);
           // return lon [degrees], lat [degrees]
           for (unsigned int d=0; d<dim-1; ++d)
@@ -144,7 +149,8 @@ namespace aspect
     LithosphereRift<dim>::
     distance_to_polygon (const Point<dim-1> &surface_position) const
     {
-      // Inside is positive, outside negative. We assume no overlap of the different polygons.
+      // Inside the polygon is positive, outside negative. We assume the different polygons do not overlap.
+      // The Utilities function only works in 3d, so compute distance here in 2d.
       double max_distance = -1e24;
       unsigned int max_distance_polygon = 0;
       for (unsigned int n = 0; n<polygon_point_list.size(); ++n)
@@ -160,10 +166,8 @@ namespace aspect
           else
             {
               temp_distance = Utilities::signed_distance_to_polygon<dim>(polygon_point_list[n], Point<2>(surface_position[0],surface_position[dim-2]));
-//sb             std::cout << "Distance to polygon " << n << " " << surface_position << " " << temp_distance << std::endl;
             }
 
-//          std::cout << "Distance to polygon " << dim << " " << surface_position << " " << temp_distance << std::endl;
           if (temp_distance > max_distance)
             {
               max_distance = temp_distance;
@@ -183,58 +187,55 @@ namespace aspect
         {
           prm.declare_entry ("Standard deviation of Gaussian rift geometry", "20000",
                              Patterns::Double (0),
-                             "The standard deviation of the Gaussian distribution of the amplitude of the strain noise. "
-                             "Note that this parameter is taken to be the same for all rift segments. "
-                             "Units: $m$ or degrees.");
+                             "The standard deviation of the Gaussian distribution of the thinning/thickening "
+                             "of the lithosphere thicknesses. This parameter is taken to be the same "
+                             "for all rift segments. Units: $m$ or degrees.");
+          prm.declare_entry("Amplitude of Gaussian rift geometry", "0.2",
+                            Patterns::List(Patterns::Double(-1, 1)),
+                            "The amplitude of the Gaussian distribution of the thinning/thickening of the. "
+                            "lithosphere thicknesses. This parameter is taken to be the same for all rift segments, "
+                            "but can be set to vary per lithosphere layer. "
+                            "Units: none.");
           prm.declare_entry ("Half width of polygon smoothing", "20000",
                              Patterns::Double (0),
-                             "The half width of the hyperbolic tangent smoothing used to transition to the lithospheric thicknesses of the polygon. "
-                             "Note that this parameter is taken to be the same for all polygons. "
+                             "The half width of the hyperbolic tangent smoothing used to transition to the "
+                             "lithospheric thicknesses of the polygon. This parameter is taken to be the same for all polygons. "
                              "Units: $m$ or degrees.");
           prm.declare_entry ("Blend polygons and rifts", "true",
                              Patterns::Bool (),
-                             "Whether or not to blend the contributions of polygons and the rift. For true, they're blend together. "
-                             "For false, the polygon thicknesses are taken as the local thicknesses. "
-                             "Units: /.");
-          prm.declare_entry ("Amplitude of Gaussian rift geometry", "0.2",
-                             Patterns::List(Patterns::Double (-1,1)),
-                             "The amplitude of the Gaussian distribution of the amplitude of the strain noise. "
-                             "Note that this parameter is taken to be the same for all rift segments, but can "
-                             "vary per lithosphere layer. "
+                             "Whether or not to blend the contributions of polygons and rift segments. If true, "
+                             "they are blended, if false the polygon thicknesses are taken as the local thicknesses. "
                              "Units: none.");
-          prm.declare_entry ("Layer thicknesses", "30000.",
-                             Patterns::List(Patterns::Double(0)),
-                             "List of thicknesses for the bottom of the lithospheric layers,"
-                             "for a total of N+1 values, where N is the number of compositional fields."
-                             "If only one value is given, then all use the same value.  Units: $m$");
-          prm.declare_entry ("Rift axis line segments",
-                             "",
-                             Patterns::Anything(),
-                             "Set the line segments that represent the rift axis. Each segment is made up of "
-                             "two points that represent horizontal coordinates (x,y) or (lon,lat). "
-                             "The exact format for the point list describing the segments is "
-                             "\"x1,y1>x2,y2;x2,y2>x3,y3;x4,y4>x5,y5\". Note that the segments can be connected "
-                             "or isolated. The units of the coordinates are "
-                             "dependent on the geometry model. In the box model they are in meters, in the "
-                             "chunks they are in degrees.");
+          prm.declare_entry("Layer thicknesses", "30000.",
+                            Patterns::List(Patterns::Double(0)),
+                            "List of reference lithospheric layer thicknesses, i.e., the thicknesses of "
+                            "the upper crust, lower crust and lithospheric mantle layers. "
+                            "Units: $m$");
+          prm.declare_entry("Rift axis line segments",
+                            "",
+                            Patterns::Anything(),
+                            "The line segments that represent the rift axis separated by a semi-colon. "
+                            "Each segment is made up of two points that represent horizontal coordinates (x,y) or (lon,lat). "
+                            "The exact format for the point list describing the segments is "
+                            "\"x1,y1>x2,y2;x2,y2>x3,y3;x4,y4>x5,y5\". Note that the segments can be connected "
+                            "or isolated. The units of the coordinates are "
+                            "dependent on the geometry model. In the box model they are in meters, in the "
+                            "chunks they are in degrees. Units: $m$ or degrees.");
           prm.declare_entry ("Lithospheric polygons",
                              "",
                              Patterns::List(Patterns::Anything()),
-                             "Set the polygons that represent an area of different lithospheric thickness. "
-                             "The polygons are separated by semicolons."
-                             "Each polygon is a list of "
+                             "The points making up polygons that represent an area of different lithospheric thickness. "
+                             "The polygons are separated by semicolons. Each polygon is a list of "
                              "points that represent horizontal coordinates (x,y) or (lon,lat). "
                              "The exact format for the point list describing a polygon is "
                              "\"x1,y1>x2,y2>x3,y3>x4,y4>x5,y5\". Note that the polygon is assumed to be closed. "
-                             "The units of the coordinates are "
-                             "dependent on the geometry model. In the box model they are in meters, in the "
-                             "chunks they are in degrees.");
+                             "The units of the coordinates are dependent on the geometry model. "
+                             "In the box model they are in meters, in the chunks they are in degrees. Units: $m$ or degrees.");
           prm.declare_entry ("Lithospheric polygon layer thicknesses", "30000.",
                              Patterns::List(Patterns::List(Patterns::Double(0),0,3,","),0,10,";"),
                              "List of thicknesses of the lithospheric layers for each polygon."
-                             "For each polygon a total of 3 values should be given (upper crust, lower crust, mantle lithosphere)."
-                             "If only one value is given, then all use the same value.  Units: $m$");
-
+                             "For each polygon, a total of 3 thicknesses should be given (upper crust, lower crust, mantle lithosphere)."
+                             "If only one value is given, then all layers are assigned the same value. Units: $m$");
         }
         prm.leave_subsection();
       }
@@ -246,54 +247,57 @@ namespace aspect
     LithosphereRift<dim>::parse_parameters (ParameterHandler &prm)
     {
       // Check that the required compositional fields exist.
-      AssertThrow(this->introspection().compositional_name_exists("upper"),ExcMessage("We need a compositional field called 'upper' representing the upper crust."));
-      AssertThrow(this->introspection().compositional_name_exists("lower"),ExcMessage("We need a compositional field called 'lower' representing the lower crust."));
-      AssertThrow(this->introspection().compositional_name_exists("mantle_L"),ExcMessage("We need a compositional field called 'mantle_L' representing the lithospheric part of the mantle."));
+      AssertThrow(this->introspection().compositional_name_exists("upper"),
+                  ExcMessage("We need a compositional field called 'upper' representing the upper crust."));
+      AssertThrow(this->introspection().compositional_name_exists("lower"),
+                  ExcMessage("We need a compositional field called 'lower' representing the lower crust."));
+      AssertThrow(this->introspection().compositional_name_exists("mantle_L"),
+                  ExcMessage("We need a compositional field called 'mantle_L' representing the lithospheric part of the mantle."));
 
       prm.enter_subsection ("Initial composition model");
       {
         prm.enter_subsection("Lithosphere with rift");
         {
           sigma_rift             = prm.get_double ("Standard deviation of Gaussian rift geometry");
+          A_rift                 = Utilities::possibly_extend_from_1_to_N(Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
+                                                                          3,
+                                                                          "Amplitude of Gaussian rift geometry");
           sigma_polygon          = prm.get_double ("Half width of polygon smoothing");
           blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
-          A                      = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
+          reference_thicknesses  = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
                                                                            3,
-                                                                           "Amplitude of Gaussian rift geometry");
-          thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
-                                                                3,
-                                                                "Layer thicknesses");
+                                                                           "Layer thicknesses");
           // Read in the string of segments
           const std::string temp_all_segments = prm.get("Rift axis line segments");
           // Split the string into segment strings
           const std::vector<std::string> temp_segments = Utilities::split_string_list(temp_all_segments,';');
           const unsigned int n_temp_segments = temp_segments.size();
-          point_list.resize(n_temp_segments);
+          rift_point_list.resize(n_temp_segments);
           // Loop over the segments to extract the points
-          for (unsigned int i_segment = 0; i_segment < n_temp_segments; i_segment++)
+          for (unsigned int i_segment = 0; i_segment < n_temp_segments; ++i_segment)
             {
               // In 3d a line segment consists of 2 points,
-              // in 2d only 1 (ridge axis orthogonal to x and y)
-
+              // in 2d of only 1 (the horizontal ridge axis runs orthogonal to x and y into the screen)
               const std::vector<std::string> temp_segment = Utilities::split_string_list(temp_segments[i_segment],'>');
 
               if (dim == 3)
                 {
-                  AssertThrow(temp_segment.size() == 2,ExcMessage ("The given coordinate '" + temp_segment[i_segment] + "' is not correct. "
+                  AssertThrow(temp_segment.size() == 2,ExcMessage ("The given segment '" + temp_segment[i_segment] + "' is not correct. "
                                                                    "It should only contain 2 parts: "
                                                                    "the two points of the segment, separated by a '>'."));
                 }
               else
                 {
-                  AssertThrow(temp_segment.size() == 1,ExcMessage ("The given coordinate '" + temp_segment[i_segment] + "' is not correct. "
+                  AssertThrow(temp_segment.size() == 1,ExcMessage ("The given segment '" + temp_segment[i_segment] + "' is not correct. "
                                                                    "It should only contain 1 part: "
                                                                    "the point representing the rift axis."));
                 }
 
-              // Loop over the dim-1 points of each segment (i.e. in 2d only 1 point is required for a 'segment')
-              for (unsigned int i_points = 0; i_points < dim-1; i_points++)
+              // Loop over the dim-1 points of each segment
+              for (unsigned int i_points = 0; i_points < dim-1; ++i_points)
                 {
                   const std::vector<double> temp_point = Utilities::string_to_double(Utilities::split_string_list(temp_segment[i_points],','));
+
                   if (dim == 3)
                     {
                       AssertThrow(temp_point.size() == 2,ExcMessage ("The given coordinates of segment '" + temp_segment[i_points] + "' are not correct. "
@@ -307,13 +311,14 @@ namespace aspect
                                                                      "the one coordinate of the segment end point."));
                     }
 
-                  // Add the point to the list of points for this segment
-                  point_list[i_segment][i_points][0] = temp_point[0];
-                  point_list[i_segment][i_points][1] = temp_point[dim-2];
+                  // Add the point to the list of points for this segment. Two points are set
+                  // even in 2d, although in 2d they are the same.
+                  rift_point_list[i_segment][i_points][0] = temp_point[0];
+                  rift_point_list[i_segment][i_points][1] = temp_point[dim-2];
                 }
             }
 
-          // Split the string into the separate polygons
+          // Split the polygon string into the separate polygons
           const std::vector<std::string> temp_polygons = Utilities::split_string_list(prm.get("Lithospheric polygons"),';');
           const std::vector<std::string> temp_thicknesses = Utilities::split_string_list(prm.get("Lithospheric polygon layer thicknesses"),';');
           const unsigned int n_polygons = temp_polygons.size();
@@ -322,24 +327,17 @@ namespace aspect
                                  ") does not correspond to the number of polygons for which a thickness is prescribed (" +
                                  Utilities::int_to_string(temp_thicknesses.size()) + ")."));
 
-
-
           polygon_point_list.resize(n_polygons);
           polygon_thicknesses.resize(n_polygons);
 
           for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
             {
               polygon_thicknesses[i_polygons] = Utilities::string_to_double(Utilities::split_string_list(temp_thicknesses[i_polygons],','));
-              AssertThrow(polygon_thicknesses[i_polygons].size()==3,
+              AssertThrow(polygon_thicknesses[i_polygons].size() == 3,
                           ExcMessage ("The number of layer thicknesses should be equal to 3 for polygon: " + Utilities::int_to_string(i_polygons) +
                                       " but it is " + Utilities::int_to_string(polygon_thicknesses[i_polygons].size())));
 
-//sb              std::cout << "polygon thicknesses ";
-//sb              for (unsigned int q=0; q<polygon_thicknesses[i_polygons].size(); ++q)
-//sb                std::cout << polygon_thicknesses[i_polygons][q] << " ";
-//sb              std::cout << std::endl;
-
-              // Split the string into point strings
+              // Split the polygon string into point strings
               const std::vector<std::string> temp_points = Utilities::split_string_list(temp_polygons[i_polygons],'>');
               const unsigned int n_temp_points = temp_points.size();
               if (dim == 3)
@@ -350,9 +348,11 @@ namespace aspect
                 {
                   AssertThrow(n_temp_points==2, ExcMessage ("The number of polygon points should be equal to 2 in 2d."));
                 }
+
               polygon_point_list[i_polygons].resize(n_temp_points);
-              // Loop over the points of the polygon. Each point should consist of 2 values (lon and lat coordinate).
-              for (unsigned int i_points = 0; i_points < n_temp_points; i_points++)
+
+              // Loop over the points of the polygon. Each point coordinate should consist of 2 (in 3d) or 1 (in 2d) values.
+              for (unsigned int i_points = 0; i_points < n_temp_points; ++i_points)
                 {
                   const std::vector<double> temp_point = Utilities::string_to_double(Utilities::split_string_list(temp_points[i_points],','));
                   AssertThrow(temp_point.size() == dim-1,ExcMessage ("The given coordinates of point '" + temp_points[i_points] + "' are not correct. "
@@ -363,6 +363,8 @@ namespace aspect
                   polygon_point_list[i_polygons][i_points][0] = temp_point[0];
                   polygon_point_list[i_polygons][i_points][1] = temp_point[dim-2];
                 }
+
+              // For simplicity later on, we want the polygon coordinates of each point in 2d to be increasing.
               if  (dim == 2)
                 AssertThrow(polygon_point_list[i_polygons][0][0] < polygon_point_list[i_polygons][1][0], ExcMessage("The order of the x coordinates of the 2 points "
                             "of each 2d polygon should be ascending. "));
@@ -385,12 +387,13 @@ namespace aspect
     ASPECT_REGISTER_INITIAL_COMPOSITION_MODEL(LithosphereRift,
                                               "lithosphere with rift",
                                               "A class that implements initial conditions for a continental rift "
-                                              "by computing the thickness of the upper crust, lower crust and mantle "
-                                              "lithosphere layers. This thickness decreases towards the axis of the "
+                                              "by computing the variable thickness of the upper crust, lower crust and mantle "
+                                              "lithosphere layers. Thicknesses can change towards the axis of the "
                                               "rift according to a Gaussian distribution whose amplitude and standard "
                                               "deviation can be specified from the input file. "
                                               "Additional variations in layer thicknesses can be introduced through the "
                                               "addition of polygons. Note that the different polygons "
-                                              "are assumed not to overlap. ")
+                                              "are assumed not to overlap. The user can decide how overlapping rifts "
+                                              "and polygons are treated. ")
   }
 }
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
index 267914645ba..dbd5902e0bc 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
@@ -1,5 +1,5 @@
 /*
-  Copyright (C) 2017 by the authors of the ASPECT code.
+  Copyright (C) 2023 by the authors of the ASPECT code.
 
   This file is part of ASPECT.
 
@@ -60,17 +60,18 @@ namespace aspect
                                     const unsigned int compositional_index) const;
 
         /**
-         * Return the overall shortest distance to the rift segments
+         * Return the overall shortest distance to the rift center segments.
          */
         double distance_to_rift (const Point<dim-1> &position) const;
 
         /*
-         * Return the overall shortest distance to the polygon segments
+         * Return the overall shortest distance to the polygon segments. Polygons
+         * can be used to specify lithosphere of different thicknesses.
          */
         std::pair<double,unsigned int> distance_to_polygon (const Point<dim-1> &position) const;
 
         /*
-         * Return the position of the point in surface coordinates
+         * Return the position of the point in surface coordinates,
          * i.e. x(,y) in meters or lon(,lat) in degrees.
          */
         Point<dim-1> surface_position (const Point<dim> &position,
@@ -93,11 +94,23 @@ namespace aspect
       private:
 
         /**
-         * The standard deviation of the Gaussian amplitude of the lithospheric thicknesses
-         * with distance from the rift axis.
+         * The standard deviation of the rift-perpendicular Gaussian distribution
+         * of the thinning/thickening of the lithospheric thicknesses with its
+         * maximum along the rift axis.
          */
         double sigma_rift;
 
+        /**
+         * The maximum amplitude of the Gaussian distribution of the thinning/thickening
+         * of the lithospheric thicknesses with distance from the rift axis.
+         * The amplitude should have values between -1 and 1, where positive
+         * numbers represent a reduction in thickness and negative numbers an increase.
+         * For example, values of 0.25, 0, 0 reduce the reference thickness of the
+         * upper crust by 25%, while the lower crust and mantle lithosphere are
+         * untouched.
+         */
+        std::vector<double> A_rift;
+
         /**
          * The half width of the hyperbolic tangent used to smooth the transitions
          * between reference and polygon lithospheric thicknesses.
@@ -110,38 +123,30 @@ namespace aspect
          */
         bool blend_rift_and_polygon;
 
-        /**
-         * The maximum amplitude of the Gaussian distribution of the lithospheric thicknesses
-         * with distance from the rift axis. It should have values between -1 and 1, where positive
-         * numbers represent a reduction in thickness and negative numbers an increase.
-         */
-        std::vector<double> A;
-
         /**
          * The list of line segments consisting of two 2d coordinates per segment.
          * The segments represent the rift axis.
          */
-        std::vector<std::array<Point<2>,2 > > point_list;
+        std::vector<std::array<Point<2>,2 >> rift_point_list;
 
         /**
          * The list of lists of polygon points.
-         * The polygon represents an area of different lithospheric thicknesses.
+         * The polygons can represent areas of different lithospheric thicknesses.
          */
-        std::vector<std::vector<Point<2> > > polygon_point_list;
+        std::vector<std::vector<Point<2>>> polygon_point_list;
 
         /**
-         * Vector for the reference field thicknesses away from the rift.
+         * Vector for the reference field thicknesses away from rift and polygons.
          */
-        std::vector<double> thicknesses;
+        std::vector<double> reference_thicknesses;
 
         /**
-         * Vector for the field thicknesses inside the polygons.
+         * Vector for the field thicknesses for each polygon.
          */
-        std::vector<std::vector<double> > polygon_thicknesses;
-
+        std::vector<std::vector<double>> polygon_thicknesses;
     };
   }
 }
 
 
-#endif
+#endiff

From 893bcbea92a7705bf375bcdee44cf15cf4060f83 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Tue, 2 Jan 2024 19:40:50 +0100
Subject: [PATCH 12/38] Clean up IT

---
 .../lithosphere_rift_IT.h                     | 49 ++++++++++++-------
 .../lithosphere_rift_IT_2.cc                  |  8 +--
 2 files changed, 34 insertions(+), 23 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
index 24cc4c3fff4..cc40a4f4689 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
@@ -83,6 +83,7 @@ namespace aspect
         parse_parameters (ParameterHandler &prm);
 
       private:
+
         /**
          * Surface temperature
          */
@@ -94,48 +95,58 @@ namespace aspect
         double LAB_isotherm;
 
         /**
-         * Wheter or not to take the polygon thicknesses as dominant, or to smooth them
-         * gradually into rift areas.
-         */
-        bool blend_rift_and_polygon;
-
-        /**
-         * Vector for field heat production rates.
+         * Vector for lithospheric layer heat production rates.
          */
         std::vector<double> heat_productivities;
 
         /**
-         * Vector for thermal conductivities.
+         * Vector for lithospheric layer thermal conductivities.
          */
         std::vector<double> conductivities;
 
         /**
-         * Vector for field densities.
+         * Vector for lithospheric layer densities.
          */
         std::vector<double> densities;
 
         /**
          * Vector for the reference field thicknesses.
          */
-        std::vector<double> thicknesses;
+        std::vector<double> reference_thicknesses;
 
         /**
-         * Vector for the reference field thicknesses away from the rift.
+         * The standard deviation of the Gaussian distribution of the lithospheric thicknesses
+         * around the rift segments.
          */
-        std::vector<std::vector<double> > polygon_thicknesses;
+        double sigma_rift;
 
         /**
-         * The standard deviation of the Gaussian amplitude of the lithospheric thicknesses.
+         * The maximum amplitude of the Gaussian distribution of the thinning/thickening
+         * of the lithospheric thicknesses with distance from the rift axis.
+         * The amplitude should have values between -1 and 1, where positive
+         * numbers represent a reduction in thickness and negative numbers an increase.
+         * For example, values of 0.25, 0, 0 reduce the reference thickness of the
+         * upper crust by 25%, while the lower crust and mantle lithosphere are
+         * untouched.
+         */
+        std::vector<double> A_rift;
+
+        /**
+         * Vector for the polygon thicknesses.
+         */
+        std::vector<std::vector<double>> polygon_thicknesses;
+
+        /**
+         * The half width of the hyperbolic tangent used to smooth the transitions
+         * between reference and polygon lithospheric thicknesses.
          */
-        double sigma_rift;
         double sigma_polygon;
 
         /**
-         * The maximum amplitude of the Gaussian distribution of the lithospheric thicknesses
-         * with distance from the rift axis. It should have values between -1 and 1, where positive
-         * numbers represent a reduction in thickness and negative numbers an increase.
+         * Whether or not to take the polygon thicknesses as dominant, or to smooth them
+         * gradually into rift areas.
          */
-        std::vector<double> A;
+        bool blend_rift_and_polygon;
 
         /**
          * Whether or not to use a compensation depth for the temperature
@@ -168,4 +179,4 @@ namespace aspect
 }
 
 
-#endif
+#endif
\ No newline at end of file
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index 9c6c084f5bc..bbbb42872db 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -93,15 +93,15 @@ namespace aspect
       local_thicknesses[0] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][0]
                               +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[0])
                              *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+                               (1.0 - A_rift[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
       local_thicknesses[1] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
                               +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
                              *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+                               (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
       local_thicknesses[2] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
                               +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
                              *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+                               (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
 
       const double depth = this->get_geometry_model().depth(position);
 
@@ -196,7 +196,7 @@ namespace aspect
           sigma_rift           = prm.get_double ("Standard deviation of Gaussian rift geometry");
           sigma_polygon        = prm.get_double ("Half width of polygon smoothing");
           blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
-          A                    = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
+          A_rift                = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
                                                                          3,
                                                                          "Amplitude of Gaussian rift geometry");
           thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),

From 2f60c80c1eaca82c53e6700a764b1536bcf79366 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Mon, 15 Jan 2024 09:49:45 +0100
Subject: [PATCH 13/38] Clean up IT

---
 .../lithosphere_rift_IT.h                     |   6 +
 .../lithosphere_rift_IT_2.cc                  | 103 ++++++++++--------
 2 files changed, 65 insertions(+), 44 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
index cc40a4f4689..0d3d2b4dfdb 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
@@ -174,6 +174,12 @@ namespace aspect
          * Vector containing the names of the compositional fields.
          */
         std::vector<std::string> list_of_composition_names;
+
+        /**
+         * Whether a cartesian box geometry is used, or a geometry
+         * of spherical type (e.g., shell or chunk).
+         */
+        bool cartesian_geometry;
     };
   }
 }
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index bbbb42872db..cfd0290ed22 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -44,22 +44,27 @@ namespace aspect
     initialize ()
     {
 
-      // Check that the required radioactive heating model ("compositional heating") is used
+      // Check that the required radioactive heating model ("compositional heating") is used.
       const std::vector<std::string> &heating_models = this->get_heating_model_manager().get_active_heating_model_names();
       AssertThrow(std::find(heating_models.begin(), heating_models.end(), "compositional heating") != heating_models.end(),
                   ExcMessage("The lithosphere with rift initial temperature plugin requires the compositional heating plugin."));
 
-      // Check that the required material model ("visco plastic") is used
-      //AssertThrow((dynamic_cast<MaterialModel::ViscoPlasticStrain<dim> *> (const_cast<MaterialModel::Interface<dim> *>(&this->get_material_model()))) != 0,
-      AssertThrow((dynamic_cast<MaterialModel::ViscoPlastic<dim> *> (const_cast<MaterialModel::Interface<dim> *>(&this->get_material_model()))) != 0,
+      // Check that the required material model ("visco plastic") is used.
+      AssertThrow(Plugins::plugin_type_matches<const MaterialModel::ViscoPlastic<dim>> (this->get_material_model()),
                   ExcMessage("The lithosphere with rift initial temperature plugin requires the viscoplastic material model plugin."));
 
       // The simulator only keeps the initial conditions around for
       // the first time step. As a consequence, we have to save a
-      // shared pointer to that object ourselves the first time we get
-      // here.
+      // shared pointer to that object ourselves the first time we get here.
       if (initial_composition_manager == nullptr)
         initial_composition_manager = this->get_initial_composition_manager_pointer();
+
+      // Check that the required initial composition model is used.
+      AssertThrow(initial_composition_manager->template has_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>(),
+      ExcMessage("The initial temperature plugin lithosphere with rift requires the correspond initial composition plugin."));
+
+      // Determine whether a cartesian or a spherical geometry is used.
+      cartesian_geometry = dynamic_cast<const GeometryModel::Box<dim> *>(&this->get_geometry_model()) != NULL ? true : false;
     }
 
 
@@ -69,40 +74,43 @@ namespace aspect
     initial_temperature (const Point<dim> &position) const
     {
       // Determine coordinate system
-      const bool cartesian_geometry = dynamic_cast<const GeometryModel::Box<dim> *>(&this->get_geometry_model()) != NULL ? true : false;
+      //const bool cartesian_geometry = dynamic_cast<const GeometryModel::Box<dim> *>(&this->get_geometry_model()) != NULL ? true : false;
 
       // Get the distance to the line segments along a path parallel to the surface
-      //InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> (const_cast<InitialComposition::Interface<dim> *>(&this->get_initial_composition()));
-
       double distance_to_rift_axis = 1e23;
       Point<dim-1> surface_position;
       std::pair<double, unsigned int> distance_to_L_polygon;
-      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim>>>::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
-           it != initial_composition_manager->get_active_initial_composition_conditions().end();
-           ++it)
-        if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
-          {
-            surface_position = ic->surface_position(position, cartesian_geometry);
-            distance_to_rift_axis = ic->distance_to_rift(surface_position);
-            distance_to_L_polygon = ic->distance_to_polygon(surface_position);
-          }
+      // Get the initial composition plugin
+      const InitialComposition::LithosphereRift<dim> &ic = initial_composition_manager->template get_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>();
+      //for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim>>>::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
+      //     it != initial_composition_manager->get_active_initial_composition_conditions().end();
+      //     ++it)
+      //  if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
+      //    {
+            surface_position = ic.surface_position(position, cartesian_geometry);
+            distance_to_rift_axis = ic.distance_to_rift(surface_position);
+            distance_to_L_polygon = ic.distance_to_polygon(surface_position);
+      //    }
 
       // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
       // based on the distance from the rift axis.
       std::vector<double> local_thicknesses(3);
-      local_thicknesses[0] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][0]
-                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[0])
-                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A_rift[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-      local_thicknesses[1] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
-                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
-                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-      local_thicknesses[2] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
-                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
+      for (unsigned int i = 0; i<3; ++i)
+      local_thicknesses[i] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][i]
+                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[i])
                              *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-
+                               (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+
+      // local_thicknesses[1] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
+      //                         +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
+      //                        *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
+      //                          (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      // local_thicknesses[2] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
+      //                         +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
+      //                        *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
+      //                          (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+
+      // Get depth with respect to the surface.
       const double depth = this->get_geometry_model().depth(position);
 
       return temperature(depth, local_thicknesses);
@@ -135,11 +143,13 @@ namespace aspect
       // Temperature in layer 3
       else if (depth < layer_thicknesses[0]+layer_thicknesses[1]+layer_thicknesses[2])
         return (LAB_isotherm-T2)/layer_thicknesses[2] *(depth-layer_thicknesses[0]-layer_thicknesses[1]) + T2;
-      // Return a constant sublithospheric temperature of .
-      // This way we can combine the continental geotherm with an adiabatic profile from the input file
-      // using the "if valid" operator on the "List of initial temperature models"
+      // Temperature in the sublithospheric mantle up to the user-set compensation depth
+      // equals the temperature at the lithosphere-asthenosphere boundary.
       else if (use_compensation_depth && depth < compensation_depth)
         return LAB_isotherm;
+      // Return a NaN sublithospheric temperature.
+      // This way we can combine the continental geotherm with an adiabatic profile from the input file
+      // using the "if valid" operator on the "List of initial temperature models".
       else
         return std::numeric_limits<double>::quiet_NaN();
     }
@@ -153,23 +163,26 @@ namespace aspect
       {
         prm.enter_subsection("Lithosphere with rift");
         {
-
           prm.declare_entry ("Surface temperature", "273.15",
                              Patterns::Double (0),
                              "The value of the surface temperature. Units: Kelvin.");
           prm.declare_entry ("LAB isotherm temperature", "1673.15",
                              Patterns::Double (0),
                              "The value of the isothermal boundary temperature assumed at the LAB "
-                             "and up to the reference depth . Units: Kelvin.");
+                             "and up to the compensation depth when this compensation is set. Units: Kelvin.");
           prm.declare_entry ("Use temperature compensation depth", "false",
                              Patterns::Bool (),
                              "Whether or not to use a compensation depth to which the LAB isotherm temperature "
-                             "is prescribed when no lithosphere is present. Below this depth, 10 times the isotherm "
-                             "is prescribed . Units: -.");
-          prm.declare_entry ("Temperature compensation depth", "100e3",
+                             "is prescribed below the lithosphere. If true, this plugin can be combined with "
+                             "the adabiatic temperature plugin. The adiabtic surface temperature can be used to "
+                             "match the LAB temperature and the adiabatic temperature at the compensation depth. "
+                             "If false, combining this plugin with the adiabtic temperature plugin will lead to "
+                             "jumps in the temperature profile at the LAB when the lithospheric thickness varies "
+                             "laterally. Units: -.");
+          prm.declare_entry ("Temperature compensation depth", "120e3",
                              Patterns::Double (0),
-                             "The depth of the temperature compensation depth, "
-                             "i.e. the depth up to which the LAB isotherm is prescribed when not in the lithosphere. Units: Kelvin.");
+                             "The depth of the temperature compensation, i.e. the depth up to which the LAB isotherm "
+                             "is prescribed below the lithosphere. Units: Kelvin.");
         }
         prm.leave_subsection();
       }
@@ -193,13 +206,13 @@ namespace aspect
       {
         prm.enter_subsection("Lithosphere with rift");
         {
-          sigma_rift           = prm.get_double ("Standard deviation of Gaussian rift geometry");
-          sigma_polygon        = prm.get_double ("Half width of polygon smoothing");
+          sigma_rift             = prm.get_double ("Standard deviation of Gaussian rift geometry");
+          sigma_polygon          = prm.get_double ("Half width of polygon smoothing");
           blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
-          A_rift                = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
+          A_rift                 = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
                                                                          3,
                                                                          "Amplitude of Gaussian rift geometry");
-          thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
+          reference_thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
                                                                 3,
                                                                 "Layer thicknesses");
           // Split the string into the separate polygons
@@ -336,6 +349,8 @@ namespace aspect
                                               "This is a temperature initial condition that "
                                               "computes a continental geotherm based on the "
                                               "conductive equations of Turcotte and Schubert Ch. 4.6. "
+                                              "This plugin only works with the corresponding composition "
+                                              "initial conditions plugin 'lithosphere with rift'. "
                                               "The geotherm can be computed for any number of crustal "
                                               "layers, for each of which a density, heat production and thermal "
                                               "conductivity should be supplied. "

From 5d382362fc8184163cf818b4363da9b660429ab5 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Mon, 15 Jan 2024 09:50:45 +0100
Subject: [PATCH 14/38] Fix type

---
 .../initial_conditions_continental_rift/lithosphere_rift_IC.h   | 2 +-
 1 file changed, 1 insertion(+), 1 deletion(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
index dbd5902e0bc..e5623570170 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
@@ -149,4 +149,4 @@ namespace aspect
 }
 
 
-#endiff
+#endif

From 4bf53aac3b97576cfa03fcec9622795b3d083c97 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Mon, 15 Jan 2024 18:05:36 +0100
Subject: [PATCH 15/38] Astyle

---
 .../lithosphere_rift_topo.cc                                  | 2 +-
 .../lithosphere_rift_topo.h                                   | 2 +-
 .../rift_box_initial_plastic_strain.cc                        | 4 ++--
 .../rift_box_initial_plastic_strain.h                         | 2 +-
 4 files changed, 5 insertions(+), 5 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
index 50556895053..eb97a691a33 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -151,7 +151,7 @@ namespace aspect
       // Get the distance to the line segments along a path parallel to the surface
       double distance_to_rift_axis = 1e23;
       std::pair<double,unsigned int> distance_to_L_polygon;
-      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim> > >::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
+      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim>>>::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
            it != initial_composition_manager->get_active_initial_composition_conditions().end();
            ++it)
         if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
index d6f6411daae..5e8a7937e1a 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
@@ -137,7 +137,7 @@ namespace aspect
         /**
          * Vector for the polygon thicknesses at the center.
          */
-        std::vector<std::vector<double> > polygon_thicknesses;
+        std::vector<std::vector<double>> polygon_thicknesses;
 
         /**
          * The maximum topography in this model
diff --git a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
index 54b46f0db46..4749c0e9752 100644
--- a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
+++ b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
@@ -37,7 +37,7 @@ namespace aspect
     void
     RiftBoxInitialPlasticStrain<dim>::initialize ()
     {
-      AssertThrow(Plugins::plugin_type_matches<MaterialModel::ViscoPlastic<dim> >(this->get_material_model()),
+      AssertThrow(Plugins::plugin_type_matches<MaterialModel::ViscoPlastic<dim>>(this->get_material_model()),
                   ExcMessage("This initial condition only makes sense in combination with the visco_plastic material model."));
 
 
@@ -196,7 +196,7 @@ namespace aspect
                   ExcMessage("This plugin requires a compositional field named plastic_strain. "));
       strain_composition_number = this->introspection().compositional_index_for_name("plastic_strain");
 
-      AssertThrow(Plugins::plugin_type_matches<GeometryModel::Box<dim> >(this->get_geometry_model()),
+      AssertThrow(Plugins::plugin_type_matches<GeometryModel::Box<dim>>(this->get_geometry_model()),
                   ExcMessage("This initial condition only makes sense in combination with the box geometry model."));
 
       // Get the number of mesh cells in each direction
diff --git a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
index 8413f4ccb3d..d8bdd7329af 100644
--- a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
+++ b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
@@ -115,7 +115,7 @@ namespace aspect
          * The list of line segments consisting of two 2d coordinates per segment (even in 2d).
          * The segments represent the rift axis.
          */
-        std::vector<std::array<Point<2>,2 > > point_list;
+        std::vector<std::array<Point<2>,2 >> point_list;
 
         /**
          * A table with random noise for the

From 9a3c9c5316aa51f605579d6a81122ca2fa126769 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Tue, 16 Jan 2024 09:15:58 +0100
Subject: [PATCH 16/38] Indent

---
 .../CMakeLists.txt                            |  2 +-
 .../initial_conditions_continental_rift.prm   | 28 +++----
 .../lithosphere_rift_IC.cc                    | 54 +++++++-------
 .../lithosphere_rift_IT.h                     |  2 +-
 .../lithosphere_rift_IT_2.cc                  | 73 +++++++------------
 5 files changed, 71 insertions(+), 88 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/CMakeLists.txt b/cookbooks/initial_conditions_continental_rift/CMakeLists.txt
index 5763297edab..9d718c97571 100644
--- a/cookbooks/initial_conditions_continental_rift/CMakeLists.txt
+++ b/cookbooks/initial_conditions_continental_rift/CMakeLists.txt
@@ -35,7 +35,7 @@ DEAL_II_INITIALIZE_CACHED_VARIABLES()
 SET(TARGET "initial_conditions_continental_rift")
 PROJECT(${TARGET})
 
-ADD_LIBRARY(${TARGET} SHARED 
+ADD_LIBRARY(${TARGET} SHARED
 lithosphere_rift_IC.cc
 lithosphere_rift_IT_2.cc
 lithosphere_rift_topo.cc
diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
index 2859f28ae40..4ef594afbaa 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
@@ -141,36 +141,36 @@ subsection Initial composition model
     set Standard deviation of Gaussian rift geometry   = 60e3
     set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
     # LAB at 110 km
-    set Rift axis line segments                        = 350e3  
+    set Rift axis line segments                        = 350e3
     set Layer thicknesses                              = 20e3, 15e3, 85e3
-   
+
     # Polygon LAB at 200 km
     set Lithospheric polygon layer thicknesses         = 23e3, 20e3 , 157.e3
     set Lithospheric polygons                          = 450e3 > 3000e3
-    set Half width of polygon smoothing                = 10e3 
+    set Half width of polygon smoothing                = 10e3
   end
-  
-  # Inherited noise 
+
+  # Inherited noise
   subsection Rift box initial plastic strain
-    set Standard deviation of Gaussian noise amplitude distribution 	= 200e3    
+    set Standard deviation of Gaussian noise amplitude distribution   = 200e3
     set Maximum amplitude of Gaussian noise amplitude distribution      = 0.250000
     set Random number generator seed                                    = 2.000000
-    set Depth around which Gaussian noise is smoothed out               = 50e3      
-    set Halfwidth with which Gaussian noise is smoothed out in depth    = 10e3         
+    set Depth around which Gaussian noise is smoothed out               = 50e3
+    set Halfwidth with which Gaussian noise is smoothed out in depth    = 10e3
     #set Grid intervals for noise X or radius                            = 2240
     # Add 16 intervals for the additional 5 km that is added to the grid
     # to account for initial topography
     #set Grid intervals for noise Y or longitude                         = 976 #960
     set Rift axis line segments                                         = 350e3
   end
-  
+
   subsection Function
     set Variable names = x,y
     set Function expression           = 0; \
                                         0; \
                                         0; \
-					0; \
-					0
+          0; \
+          0
   end
 #  subsection Function
 #    set Variable names      = x,y
@@ -190,8 +190,8 @@ subsection Boundary composition model
     set Function expression           = 0; \
                                         0; \
                                         0; \
-					0; \
-					0
+          0; \
+          0
   end
 end
 
@@ -252,7 +252,7 @@ subsection Initial temperature model
                                            0; \
                                            0; \
                                            0; \
-					   0; \
+             0; \
                                            if(x<23e3,1,0); \
                                            if(x>=23e3&x<43e3,1,0); \
                                            if(x>=43e3&x<200e3,1,0); \
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
index 0c32696912b..ae3309bf6ff 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
@@ -185,22 +185,22 @@ namespace aspect
       {
         prm.enter_subsection("Lithosphere with rift");
         {
-          prm.declare_entry ("Standard deviation of Gaussian rift geometry", "20000",
-                             Patterns::Double (0),
-                             "The standard deviation of the Gaussian distribution of the thinning/thickening "
-                             "of the lithosphere thicknesses. This parameter is taken to be the same "
-                             "for all rift segments. Units: $m$ or degrees.");
+          prm.declare_entry("Standard deviation of Gaussian rift geometry", "20000",
+                            Patterns::Double(0),
+                            "The standard deviation of the Gaussian distribution of the thinning/thickening "
+                            "of the lithosphere thicknesses. This parameter is taken to be the same "
+                            "for all rift segments. Units: \\si{\\meter} or degrees.");
           prm.declare_entry("Amplitude of Gaussian rift geometry", "0.2",
                             Patterns::List(Patterns::Double(-1, 1)),
                             "The amplitude of the Gaussian distribution of the thinning/thickening of the. "
                             "lithosphere thicknesses. This parameter is taken to be the same for all rift segments, "
                             "but can be set to vary per lithosphere layer. "
                             "Units: none.");
-          prm.declare_entry ("Half width of polygon smoothing", "20000",
-                             Patterns::Double (0),
-                             "The half width of the hyperbolic tangent smoothing used to transition to the "
-                             "lithospheric thicknesses of the polygon. This parameter is taken to be the same for all polygons. "
-                             "Units: $m$ or degrees.");
+          prm.declare_entry("Half width of polygon smoothing", "20000",
+                            Patterns::Double(0),
+                            "The half width of the hyperbolic tangent smoothing used to transition to the "
+                            "lithospheric thicknesses of the polygon. This parameter is taken to be the same for all polygons. "
+                            "Units: \\si{\\meter} or degrees.");
           prm.declare_entry ("Blend polygons and rifts", "true",
                              Patterns::Bool (),
                              "Whether or not to blend the contributions of polygons and rift segments. If true, "
@@ -210,7 +210,7 @@ namespace aspect
                             Patterns::List(Patterns::Double(0)),
                             "List of reference lithospheric layer thicknesses, i.e., the thicknesses of "
                             "the upper crust, lower crust and lithospheric mantle layers. "
-                            "Units: $m$");
+                            "Units: \\si{\\meter}");
           prm.declare_entry("Rift axis line segments",
                             "",
                             Patterns::Anything(),
@@ -220,22 +220,22 @@ namespace aspect
                             "\"x1,y1>x2,y2;x2,y2>x3,y3;x4,y4>x5,y5\". Note that the segments can be connected "
                             "or isolated. The units of the coordinates are "
                             "dependent on the geometry model. In the box model they are in meters, in the "
-                            "chunks they are in degrees. Units: $m$ or degrees.");
-          prm.declare_entry ("Lithospheric polygons",
-                             "",
-                             Patterns::List(Patterns::Anything()),
-                             "The points making up polygons that represent an area of different lithospheric thickness. "
-                             "The polygons are separated by semicolons. Each polygon is a list of "
-                             "points that represent horizontal coordinates (x,y) or (lon,lat). "
-                             "The exact format for the point list describing a polygon is "
-                             "\"x1,y1>x2,y2>x3,y3>x4,y4>x5,y5\". Note that the polygon is assumed to be closed. "
-                             "The units of the coordinates are dependent on the geometry model. "
-                             "In the box model they are in meters, in the chunks they are in degrees. Units: $m$ or degrees.");
-          prm.declare_entry ("Lithospheric polygon layer thicknesses", "30000.",
-                             Patterns::List(Patterns::List(Patterns::Double(0),0,3,","),0,10,";"),
-                             "List of thicknesses of the lithospheric layers for each polygon."
-                             "For each polygon, a total of 3 thicknesses should be given (upper crust, lower crust, mantle lithosphere)."
-                             "If only one value is given, then all layers are assigned the same value. Units: $m$");
+                            "chunks they are in degrees. Units: \\si{\\meter} or degrees.");
+          prm.declare_entry("Lithospheric polygons",
+                            "",
+                            Patterns::List(Patterns::Anything()),
+                            "The points making up polygons that represent an area of different lithospheric thickness. "
+                            "The polygons are separated by semicolons. Each polygon is a list of "
+                            "points that represent horizontal coordinates (x,y) or (lon,lat). "
+                            "The exact format for the point list describing a polygon is "
+                            "\"x1,y1>x2,y2>x3,y3>x4,y4>x5,y5\". Note that the polygon is assumed to be closed. "
+                            "The units of the coordinates are dependent on the geometry model. "
+                            "In the box model they are in meters, in the chunks they are in degrees. Units: \\si{\\meter} or degrees.");
+          prm.declare_entry("Lithospheric polygon layer thicknesses", "30000.",
+                            Patterns::List(Patterns::List(Patterns::Double(0), 0, 3, ","), 0, 10, ";"),
+                            "List of thicknesses of the lithospheric layers for each polygon."
+                            "For each polygon, a total of 3 thicknesses should be given (upper crust, lower crust, mantle lithosphere)."
+                            "If only one value is given, then all layers are assigned the same value. Units: \\si{\\meter}");
         }
         prm.leave_subsection();
       }
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
index 0d3d2b4dfdb..cbb9ed56d38 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
@@ -185,4 +185,4 @@ namespace aspect
 }
 
 
-#endif
\ No newline at end of file
+#endiff
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index cfd0290ed22..7f861bcf88e 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -61,7 +61,7 @@ namespace aspect
 
       // Check that the required initial composition model is used.
       AssertThrow(initial_composition_manager->template has_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>(),
-      ExcMessage("The initial temperature plugin lithosphere with rift requires the correspond initial composition plugin."));
+                  ExcMessage("The initial temperature plugin lithosphere with rift requires the correspond initial composition plugin."));
 
       // Determine whether a cartesian or a spherical geometry is used.
       cartesian_geometry = dynamic_cast<const GeometryModel::Box<dim> *>(&this->get_geometry_model()) != NULL ? true : false;
@@ -73,42 +73,24 @@ namespace aspect
     LithosphereRift<dim>::
     initial_temperature (const Point<dim> &position) const
     {
-      // Determine coordinate system
-      //const bool cartesian_geometry = dynamic_cast<const GeometryModel::Box<dim> *>(&this->get_geometry_model()) != NULL ? true : false;
-
       // Get the distance to the line segments along a path parallel to the surface
       double distance_to_rift_axis = 1e23;
       Point<dim-1> surface_position;
       std::pair<double, unsigned int> distance_to_L_polygon;
       // Get the initial composition plugin
       const InitialComposition::LithosphereRift<dim> &ic = initial_composition_manager->template get_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>();
-      //for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim>>>::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
-      //     it != initial_composition_manager->get_active_initial_composition_conditions().end();
-      //     ++it)
-      //  if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
-      //    {
-            surface_position = ic.surface_position(position, cartesian_geometry);
-            distance_to_rift_axis = ic.distance_to_rift(surface_position);
-            distance_to_L_polygon = ic.distance_to_polygon(surface_position);
-      //    }
+      surface_position = ic.surface_position(position, cartesian_geometry);
+      distance_to_rift_axis = ic.distance_to_rift(surface_position);
+      distance_to_L_polygon = ic.distance_to_polygon(surface_position);
 
       // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
       // based on the distance from the rift axis.
       std::vector<double> local_thicknesses(3);
       for (unsigned int i = 0; i<3; ++i)
-      local_thicknesses[i] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][i]
-                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[i])
-                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-
-      // local_thicknesses[1] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
-      //                         +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
-      //                        *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-      //                          (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-      // local_thicknesses[2] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
-      //                         +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
-      //                        *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-      //                          (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+        local_thicknesses[i] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][i]
+                                +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[i])
+                               *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
+                                 (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
 
       // Get depth with respect to the surface.
       const double depth = this->get_geometry_model().depth(position);
@@ -163,26 +145,27 @@ namespace aspect
       {
         prm.enter_subsection("Lithosphere with rift");
         {
-          prm.declare_entry ("Surface temperature", "273.15",
-                             Patterns::Double (0),
-                             "The value of the surface temperature. Units: Kelvin.");
-          prm.declare_entry ("LAB isotherm temperature", "1673.15",
-                             Patterns::Double (0),
-                             "The value of the isothermal boundary temperature assumed at the LAB "
-                             "and up to the compensation depth when this compensation is set. Units: Kelvin.");
+          prm.declare_entry("Surface temperature", "273.15",
+                            Patterns::Double(0),
+                            "The value of the surface temperature. Units: \\si{\\kelvin}.");
+          prm.declare_entry("LAB isotherm temperature", "1673.15",
+                            Patterns::Double(0),
+                            "The value of the isothermal boundary temperature assumed at the LAB "
+                            "and up to the compensation depth when 'Use temperature compensation depth' "
+                            "is set to true. Units: \\si{\\kelvin}.");
           prm.declare_entry ("Use temperature compensation depth", "false",
                              Patterns::Bool (),
-                             "Whether or not to use a compensation depth to which the LAB isotherm temperature "
+                             "Whether or not to use a compensation depth up to which the LAB isotherm temperature "
                              "is prescribed below the lithosphere. If true, this plugin can be combined with "
-                             "the adabiatic temperature plugin. The adiabtic surface temperature can be used to "
-                             "match the LAB temperature and the adiabatic temperature at the compensation depth. "
-                             "If false, combining this plugin with the adiabtic temperature plugin will lead to "
+                             "the adabiatic temperature plugin. The adiabatic surface temperature can be adapted to "
+                             "ensure the LAB temperature and the adiabatic temperature match at the compensation depth. "
+                             "If false, combining this plugin with the adiabatic temperature plugin will lead to "
                              "jumps in the temperature profile at the LAB when the lithospheric thickness varies "
                              "laterally. Units: -.");
-          prm.declare_entry ("Temperature compensation depth", "120e3",
-                             Patterns::Double (0),
-                             "The depth of the temperature compensation, i.e. the depth up to which the LAB isotherm "
-                             "is prescribed below the lithosphere. Units: Kelvin.");
+          prm.declare_entry("Temperature compensation depth", "120e3",
+                            Patterns::Double(0),
+                            "The depth of the temperature compensation, i.e. the depth up to which the LAB isotherm "
+                            "is prescribed below the lithosphere. Units: \\si{\\meter}.");
         }
         prm.leave_subsection();
       }
@@ -210,11 +193,11 @@ namespace aspect
           sigma_polygon          = prm.get_double ("Half width of polygon smoothing");
           blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
           A_rift                 = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
-                                                                         3,
-                                                                         "Amplitude of Gaussian rift geometry");
+                                                                           3,
+                                                                           "Amplitude of Gaussian rift geometry");
           reference_thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
-                                                                3,
-                                                                "Layer thicknesses");
+                                                                          3,
+                                                                          "Layer thicknesses");
           // Split the string into the separate polygons
           const std::vector<std::string> temp_thicknesses = Utilities::split_string_list(prm.get("Lithospheric polygon layer thicknesses"),';');
           const unsigned int n_polygons = temp_thicknesses.size();

From ec5fd24aed452d838d7dd0f3026180e3f326f3b8 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Wed, 17 Jan 2024 18:05:02 +0100
Subject: [PATCH 17/38] Use function instead of cast

---
 .../lithosphere_rift_IT_2.cc                                    | 2 +-
 1 file changed, 1 insertion(+), 1 deletion(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index 7f861bcf88e..511f30ad148 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -64,7 +64,7 @@ namespace aspect
                   ExcMessage("The initial temperature plugin lithosphere with rift requires the correspond initial composition plugin."));
 
       // Determine whether a cartesian or a spherical geometry is used.
-      cartesian_geometry = dynamic_cast<const GeometryModel::Box<dim> *>(&this->get_geometry_model()) != NULL ? true : false;
+      cartesian_geometry = Plugins::plugin_type_matches<const GeometryModel::Box<dim>> (geometry_model);
     }
 
 

From b81547d5c6f9a47fc28ab6474db3367e29321be5 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 18 Jan 2024 10:05:43 +0100
Subject: [PATCH 18/38] Update comments topo

---
 .../lithosphere_rift_topo.h                   | 34 ++++++++++++-------
 1 file changed, 22 insertions(+), 12 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
index 5e8a7937e1a..463d47c7174 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
@@ -1,5 +1,5 @@
 /*
-  Copyright (C) 2016 by the authors of the ASPECT code.
+  Copyright (C) 2024 by the authors of the ASPECT code.
 
   This file is part of ASPECT.
 
@@ -33,8 +33,8 @@ namespace aspect
 
     /**
      * A class that describes an initial topography for the geometry model,
-     * by defining a set of polylines on the surface from the prm file. It
-     * sets the elevation in each Polyline to a constant value.
+     * based on isostatically balancing the thinning of lithospheric layers
+     * around a rift axis.
      */
     template <int dim>
     class LithosphereRift : public Interface<dim>,
@@ -76,8 +76,9 @@ namespace aspect
 
       private:
         /**
-         * The standard deviation of the Gaussian amplitude of the lithospheric thicknesses
-         * with distance from the rift axis.
+         * The standard deviation of the rift-perpendicular Gaussian distribution
+         * of the thinning/thickening of the lithospheric thicknesses with its
+         * maximum along the rift axis.
          */
         double sigma_rift;
 
@@ -88,11 +89,15 @@ namespace aspect
         double sigma_polygon;
 
         /**
-         * The maximum amplitude of the Gaussian distribution of the lithospheric thicknesses
-         * with distance from the rift axis. It should have values between -1 and 1, where positive
+         * The maximum amplitude of the Gaussian distribution of the thinning/thickening
+         * of the lithospheric thicknesses with distance from the rift axis.
+         * The amplitude should have values between -1 and 1, where positive
          * numbers represent a reduction in thickness and negative numbers an increase.
+         * For example, values of 0.25, 0, 0 reduce the reference thickness of the
+         * upper crust by 25%, while the lower crust and mantle lithosphere are
+         * untouched.
          */
-        std::vector<double> A;
+        std::vector<double> A_rift;
 
         /**
          * The maximum amplitude of the Gaussian distribution of the topography around the rift.
@@ -100,14 +105,19 @@ namespace aspect
         double topo_rift_amplitude;
 
         /**
-         * The reference lithospheric column used in computing the topography based on isostasy
-         * and the thickness of this column.
+         * The product of density, gravitational accelleration constant and thickness of the
+         * reference lithospheric column used in computing the topography based on isostasy.
          */
         double ref_rgh;
+
+        /**
+         * The thickness/depth of the reference lithospheric column used in computing the topography
+         * based on isostasy.
+         */
         double compensation_depth;
 
         /**
-         * Wheter or not to take the polygon thicknesses as dominant, or to smooth them
+         * Whether or not to take the polygon thicknesses as dominant, or to smooth them
          * gradually into rift areas.
          */
         bool blend_rift_and_polygon;
@@ -127,7 +137,7 @@ namespace aspect
         /**
          * Vector for the reference field thicknesses away from the rift.
          */
-        std::vector<double> thicknesses;
+        std::vector<double> reference_thicknesses;
 
         /**
          * Vector for the rift  thicknesses at the center.

From 75fc9743b95cf0441617248a3a531b9c32376faf Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 19 Jan 2024 15:49:27 +0100
Subject: [PATCH 19/38] Update topo files

---
 .../lithosphere_rift_topo.cc                  | 41 ++++++++++++++-----
 .../lithosphere_rift_topo.h                   |  3 +-
 2 files changed, 31 insertions(+), 13 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
index eb97a691a33..2f8e961a9aa 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -81,7 +81,7 @@ namespace aspect
       double rift_rgh = 0;
       rift_thicknesses = thicknesses;
       for (unsigned int l=0; l<rift_thicknesses.size(); ++l)
-        rift_thicknesses[l] *= (1.-A[l]);
+        rift_thicknesses[l] *= (1.-A_rift[l]);
 
       for (unsigned int l=0; l<3; ++l)
         rift_rgh += densities[l+1] * rift_thicknesses[l];
@@ -165,15 +165,15 @@ namespace aspect
       local_thicknesses[0] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][0]
                               +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[0])
                              *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+                               (1.0 - A_rift[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
       local_thicknesses[1] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
                               +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
                              *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+                               (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
       local_thicknesses[2] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
                               +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
                              *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+                               (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
 
       // The local lithospheric column
       double local_rgh = 0;
@@ -216,7 +216,7 @@ namespace aspect
           sigma_rift           = prm.get_double ("Standard deviation of Gaussian rift geometry");
           sigma_polygon        = prm.get_double ("Half width of polygon smoothing");
           blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
-          A                    = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
+          A_rift                 = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
                                                                          3,
                                                                          "Amplitude of Gaussian rift geometry");
           thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
@@ -247,12 +247,31 @@ namespace aspect
         prm.enter_subsection("Visco Plastic");
         {
           n_phases_for_each_composition = std::make_unique<std::vector<unsigned int>>();
-          temp_densities = Utilities::parse_map_to_double_array (prm.get("Densities"),
-                                                                 list_of_composition_names,
-                                                                 /*has_background_field=*/true,
-                                                                 "Densities",
-                                                                 true,
-                                                                 n_phases_for_each_composition);
+          
+          const std::vector<unsigned int> indices = this->introspection().chemical_composition_field_indices();
+
+          std::vector<unsigned int> n_phases_for_each_chemical_composition = {n_phases_for_each_composition[0]};
+          for (auto i : indices)
+          {
+            n_phases_for_each_chemical_composition.push_back(n_phases_for_each_composition[i + 1]);
+          }
+
+          std::vector<std::string> chemical_field_names = this->introspection().chemical_composition_field_names();
+          chemical_field_names.insert(chemical_field_names.begin(), "background");
+
+          std::vector<std::string> compositional_field_names = this->introspection().get_composition_names();
+          compositional_field_names.insert(compositional_field_names.begin(), "background");
+
+          Utilities::MapParsing::Options options(chemical_field_names, "Densities");
+          options.list_of_allowed_keys = compositional_field_names;
+          options.allow_multiple_values_per_key = true;
+          options.n_values_per_key = n_phases_for_each_chemical_composition;
+          options.check_values_per_key = (options.n_values_per_key.size() != 0);
+          options.store_values_per_key = (options.n_values_per_key.size() == 0);
+
+
+          temp_densities = Utilities::MapParsing::parse_map_to_double_array (prm.get("Densities"),
+                                                                 options);
         }
         prm.leave_subsection();
       }
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
index 463d47c7174..448c55e0035 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
@@ -122,7 +122,6 @@ namespace aspect
          */
         bool blend_rift_and_polygon;
 
-
         /**
          * The maximum amplitude of the topography of the polygon area.
          */
@@ -150,7 +149,7 @@ namespace aspect
         std::vector<std::vector<double>> polygon_thicknesses;
 
         /**
-         * The maximum topography in this model
+         * The maximum topography in this model.
          */
         double maximum_topography;
 

From f61d6d373535da3f7157d83d0bfc55f790792f5c Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 30 May 2024 03:35:36 +0200
Subject: [PATCH 20/38] Fix rift-craton interaction

---
 .../lithosphere_rift_IC.cc                    | 20 ++++---------------
 1 file changed, 4 insertions(+), 16 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
index ae3309bf6ff..a9bd8bc0800 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
@@ -65,18 +65,12 @@ namespace aspect
       const std::pair<double, unsigned int> distance_to_L_polygon = distance_to_polygon(surface_point);
 
       // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
-      // (in this exact order) based on the distance from the rift axis.
+      // (in this exact order) based on the distance from the rift axis and the polygons.
+      const double polygon_contribution = (0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon));
+      const double rift_contribution = (0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon));
       std::vector <double> local_thicknesses(3);
       for (unsigned int i = 0; i<3; ++i)
-        local_thicknesses[i] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][i]
-                                +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[i])
-                               * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-      //const double local_lower_crust_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
-      //                                            +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[1])
-      //                                           * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-      //const double local_mantle_lithosphere_thickness = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
-      //                                                   +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[2])
-      //                                                  *  (!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. : (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+        local_thicknesses[i] = (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))) * thicknesses[i] * rift_contribution + craton_contribution * polygon_thicknesses[distance_to_L_polygon.second][i];
 
       // Get depth with respect to the surface.
       const double depth = this->get_geometry_model().depth(position);
@@ -201,11 +195,6 @@ namespace aspect
                             "The half width of the hyperbolic tangent smoothing used to transition to the "
                             "lithospheric thicknesses of the polygon. This parameter is taken to be the same for all polygons. "
                             "Units: \\si{\\meter} or degrees.");
-          prm.declare_entry ("Blend polygons and rifts", "true",
-                             Patterns::Bool (),
-                             "Whether or not to blend the contributions of polygons and rift segments. If true, "
-                             "they are blended, if false the polygon thicknesses are taken as the local thicknesses. "
-                             "Units: none.");
           prm.declare_entry("Layer thicknesses", "30000.",
                             Patterns::List(Patterns::Double(0)),
                             "List of reference lithospheric layer thicknesses, i.e., the thicknesses of "
@@ -263,7 +252,6 @@ namespace aspect
                                                                           3,
                                                                           "Amplitude of Gaussian rift geometry");
           sigma_polygon          = prm.get_double ("Half width of polygon smoothing");
-          blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
           reference_thicknesses  = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
                                                                            3,
                                                                            "Layer thicknesses");

From 930a6fdf0e0351478d79bddfb5835a9069f35621 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 30 May 2024 04:52:20 +0200
Subject: [PATCH 21/38] Use the IC function for local thicknesses

---
 .../lithosphere_rift_IC.cc                    | 36 +++++++++----
 .../lithosphere_rift_IC.h                     | 13 ++---
 .../lithosphere_rift_IT_2.cc                  | 46 ++--------------
 .../lithosphere_rift_topo.cc                  | 53 +------------------
 4 files changed, 39 insertions(+), 109 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
index a9bd8bc0800..cf038c9c6ca 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
@@ -58,19 +58,9 @@ namespace aspect
       // Get the surface coordinates of the point under consideration
       const Point<dim-1> surface_point = surface_position(position, cartesian_geometry);
 
-      // Get the distance to the rift segments along a path parallel to the surface
-      const double distance_to_rift_axis = distance_to_rift(surface_point);
-
-      // Get the signed distance to potential polygons of different lithospheric thicknesses
-      const std::pair<double, unsigned int> distance_to_L_polygon = distance_to_polygon(surface_point);
-
       // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
       // (in this exact order) based on the distance from the rift axis and the polygons.
-      const double polygon_contribution = (0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon));
-      const double rift_contribution = (0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon));
-      std::vector <double> local_thicknesses(3);
-      for (unsigned int i = 0; i<3; ++i)
-        local_thicknesses[i] = (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))) * thicknesses[i] * rift_contribution + craton_contribution * polygon_thicknesses[distance_to_L_polygon.second][i];
+      const std::vector<double> local_thicknesses = compute_local_thickness(surface_points);
 
       // Get depth with respect to the surface.
       const double depth = this->get_geometry_model().depth(position);
@@ -171,6 +161,30 @@ namespace aspect
       return std::pair<double, unsigned int> (max_distance, max_distance_polygon);
     }
 
+    template <int dim>
+    std::vector<double>
+    LithosphereRift<dim>::
+    compute_local_thicknesses(const Point<dim - 1> &surface_point) const
+    {
+      // Get the distance to the rift segments along a path parallel to the surface
+      const double distance_to_rift_axis = distance_to_rift(surface_point);
+
+      // Get the signed distance to potential polygons of different lithospheric thicknesses
+      const std::pair<double, unsigned int> distance_to_L_polygon = distance_to_polygon(surface_point);
+
+      // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
+      // (in this exact order) based on the distance from the rift axis and the polygons.
+      const double polygon_contribution = (0.5 + 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon));
+      const double rift_contribution = (0.5 - 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon));
+      
+      std::vector<double> local_thicknesses(3);
+      for (unsigned int i = 0; i < 3; ++i)
+        local_thicknesses[i] = (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))) 
+        * thicknesses[i] * rift_contribution + craton_contribution * polygon_thicknesses[distance_to_L_polygon.second][i];
+      
+      return local_thicknesses;
+    }
+
     template <int dim>
     void
     LithosphereRift<dim>::declare_parameters (ParameterHandler &prm)
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
index e5623570170..2c081ec467e 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
@@ -77,6 +77,13 @@ namespace aspect
         Point<dim-1> surface_position (const Point<dim> &position,
                                        const bool cartesian_geometry) const;
 
+        /*
+         * Compute the local thicknesses of the upper and lower crust
+         * and lithospheric mantle based on the distance to the rift center
+         * and the edge of polygons.
+         */
+        std::vector<double> compute_local_thicknesses(const Point<dim> &position) const;
+
         /**
          * Declare the parameters this class takes through input files.
          */
@@ -117,12 +124,6 @@ namespace aspect
          */
         double sigma_polygon;
 
-        /**
-         * Whether or not to take the polygon thicknesses as dominant, or to smooth them
-         * gradually into rift areas.
-         */
-        bool blend_rift_and_polygon;
-
         /**
          * The list of line segments consisting of two 2d coordinates per segment.
          * The segments represent the rift axis.
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index 511f30ad148..6314d989b6c 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -73,24 +73,15 @@ namespace aspect
     LithosphereRift<dim>::
     initial_temperature (const Point<dim> &position) const
     {
-      // Get the distance to the line segments along a path parallel to the surface
-      double distance_to_rift_axis = 1e23;
-      Point<dim-1> surface_position;
-      std::pair<double, unsigned int> distance_to_L_polygon;
       // Get the initial composition plugin
       const InitialComposition::LithosphereRift<dim> &ic = initial_composition_manager->template get_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>();
-      surface_position = ic.surface_position(position, cartesian_geometry);
-      distance_to_rift_axis = ic.distance_to_rift(surface_position);
-      distance_to_L_polygon = ic.distance_to_polygon(surface_position);
+
+      // Convert to surface position
+      const Point<dim - 1> surface_position = ic.surface_position(position, cartesian_geometry);
 
       // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
-      // based on the distance from the rift axis.
-      std::vector<double> local_thicknesses(3);
-      for (unsigned int i = 0; i<3; ++i)
-        local_thicknesses[i] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][i]
-                                +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*reference_thicknesses[i])
-                               *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                                 (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      // based on the distance from the rift axis and polygon edges.
+      std::vector<double> local_thicknesses = ic.compute_local_thicknesses(surface_position);
 
       // Get depth with respect to the surface.
       const double depth = this->get_geometry_model().depth(position);
@@ -185,33 +176,6 @@ namespace aspect
       }
       prm.leave_subsection();
 
-      prm.enter_subsection ("Initial composition model");
-      {
-        prm.enter_subsection("Lithosphere with rift");
-        {
-          sigma_rift             = prm.get_double ("Standard deviation of Gaussian rift geometry");
-          sigma_polygon          = prm.get_double ("Half width of polygon smoothing");
-          blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
-          A_rift                 = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
-                                                                           3,
-                                                                           "Amplitude of Gaussian rift geometry");
-          reference_thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
-                                                                          3,
-                                                                          "Layer thicknesses");
-          // Split the string into the separate polygons
-          const std::vector<std::string> temp_thicknesses = Utilities::split_string_list(prm.get("Lithospheric polygon layer thicknesses"),';');
-          const unsigned int n_polygons = temp_thicknesses.size();
-          polygon_thicknesses.resize(n_polygons);
-          for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
-            {
-              polygon_thicknesses[i_polygons] = Utilities::string_to_double(Utilities::split_string_list(temp_thicknesses[i_polygons],','));
-              AssertThrow(polygon_thicknesses[i_polygons].size()==3, ExcMessage ("The number of layer thicknesses should be equal to 3."));
-            }
-        }
-        prm.leave_subsection();
-      }
-      prm.leave_subsection();
-
       prm.enter_subsection ("Initial temperature model");
       {
         prm.enter_subsection("Lithosphere with rift");
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
index 2f8e961a9aa..75076ace03c 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -148,32 +148,10 @@ namespace aspect
       for (unsigned int d=0; d<dim-1; ++d)
         surface_position[d] = position[d];
 
-      // Get the distance to the line segments along a path parallel to the surface
-      double distance_to_rift_axis = 1e23;
-      std::pair<double,unsigned int> distance_to_L_polygon;
-      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim>>>::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
-           it != initial_composition_manager->get_active_initial_composition_conditions().end();
-           ++it)
-        if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
-          {
-            distance_to_rift_axis = ic->distance_to_rift(surface_position);
-            distance_to_L_polygon = ic->distance_to_polygon(surface_position);
-          }
+      const InitialComposition::LithosphereRift<dim> &ic = initial_composition_manager->template get_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>();
 
       // Compute the topography based on distance to the rift and distance to the polygon
-      std::vector<double> local_thicknesses(3);
-      local_thicknesses[0] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][0]
-                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[0])
-                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A_rift[0] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-      local_thicknesses[1] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][1]
-                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[1])
-                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
-      local_thicknesses[2] = ((0.5+0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*polygon_thicknesses[distance_to_L_polygon.second][2]
-                              +(0.5-0.5*std::tanh(distance_to_L_polygon.first/sigma_polygon))*thicknesses[2])
-                             *(!blend_rift_and_polygon && distance_to_L_polygon.first > 0.-2.*sigma_polygon ? 1. :
-                               (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis,2)/(2.0*std::pow(sigma_rift,2))))));
+      std::vector<double> local_thicknesses = ic.compute_local_thicknesses(surface_position);
 
       // The local lithospheric column
       double local_rgh = 0;
@@ -209,33 +187,6 @@ namespace aspect
     void
     LithosphereRift<dim>::parse_parameters (ParameterHandler &prm)
     {
-      prm.enter_subsection ("Initial composition model");
-      {
-        prm.enter_subsection("Lithosphere with rift");
-        {
-          sigma_rift           = prm.get_double ("Standard deviation of Gaussian rift geometry");
-          sigma_polygon        = prm.get_double ("Half width of polygon smoothing");
-          blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
-          A_rift                 = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
-                                                                         3,
-                                                                         "Amplitude of Gaussian rift geometry");
-          thicknesses = Utilities::possibly_extend_from_1_to_N (Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
-                                                                3,
-                                                                "Layer thicknesses");
-          // Split the string into the separate polygons
-          const std::vector<std::string> temp_thicknesses = Utilities::split_string_list(prm.get("Lithospheric polygon layer thicknesses"),';');
-          const unsigned int n_polygons = temp_thicknesses.size();
-          polygon_thicknesses.resize(n_polygons);
-          for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
-            {
-              polygon_thicknesses[i_polygons] = Utilities::string_to_double(Utilities::split_string_list(temp_thicknesses[i_polygons],','));
-              AssertThrow(polygon_thicknesses[i_polygons].size()==3, ExcMessage ("The number of layer thicknesses should be equal to 3."));
-            }
-        }
-        prm.leave_subsection();
-      }
-      prm.leave_subsection();
-
       prm.enter_subsection ("Compositional fields");
       {
         list_of_composition_names = Utilities::split_string_list (prm.get("Names of fields"));

From fe988f88ed225a2b2e53f11ed88d2579d57a628d Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 30 May 2024 06:02:08 +0200
Subject: [PATCH 22/38] Fix overrides and parameter names

---
 .../lithosphere_rift_IC.cc                    |  4 +-
 .../lithosphere_rift_IC.h                     |  8 +-
 .../lithosphere_rift_IT.h                     |  8 +-
 .../lithosphere_rift_IT_2.cc                  |  2 +-
 .../lithosphere_rift_topo.cc                  | 81 ++++++++++++-------
 .../lithosphere_rift_topo.h                   |  8 +-
 .../rift_box_initial_plastic_strain.h         |  6 +-
 7 files changed, 69 insertions(+), 48 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
index cf038c9c6ca..5f667e72e62 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
@@ -60,7 +60,7 @@ namespace aspect
 
       // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
       // (in this exact order) based on the distance from the rift axis and the polygons.
-      const std::vector<double> local_thicknesses = compute_local_thickness(surface_points);
+      const std::vector<double> local_thicknesses = compute_local_thicknesses(surface_point);
 
       // Get depth with respect to the surface.
       const double depth = this->get_geometry_model().depth(position);
@@ -180,7 +180,7 @@ namespace aspect
       std::vector<double> local_thicknesses(3);
       for (unsigned int i = 0; i < 3; ++i)
         local_thicknesses[i] = (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))) 
-        * thicknesses[i] * rift_contribution + craton_contribution * polygon_thicknesses[distance_to_L_polygon.second][i];
+        * reference_thicknesses[i] * rift_contribution + polygon_contribution * polygon_thicknesses[distance_to_L_polygon.second][i];
       
       return local_thicknesses;
     }
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
index 2c081ec467e..80cfb48be7a 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.h
@@ -49,7 +49,7 @@ namespace aspect
          * beginning of the program. Checks preconditions.
          */
         void
-        initialize ();
+        initialize () override;
 
         /**
          * Return the initial composition as a function of position and number
@@ -57,7 +57,7 @@ namespace aspect
          */
         virtual
         double initial_composition (const Point<dim> &position,
-                                    const unsigned int compositional_index) const;
+                                    const unsigned int compositional_index) const override;
 
         /**
          * Return the overall shortest distance to the rift center segments.
@@ -82,7 +82,7 @@ namespace aspect
          * and lithospheric mantle based on the distance to the rift center
          * and the edge of polygons.
          */
-        std::vector<double> compute_local_thicknesses(const Point<dim> &position) const;
+        std::vector<double> compute_local_thicknesses(const Point<dim-1> &position) const;
 
         /**
          * Declare the parameters this class takes through input files.
@@ -96,7 +96,7 @@ namespace aspect
          */
         virtual
         void
-        parse_parameters (ParameterHandler &prm);
+        parse_parameters (ParameterHandler &prm) override;
 
       private:
 
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
index cbb9ed56d38..17d26e8af0b 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT.h
@@ -52,13 +52,13 @@ namespace aspect
          * beginning of the program. Checks preconditions.
          */
         void
-        initialize ();
+        initialize () override;
 
         /**
          * Return the initial temperature as a function of position.
          */
         virtual
-        double initial_temperature (const Point<dim> &position) const;
+        double initial_temperature (const Point<dim> &position) const override;
 
         /**
          * Return the initial temperature as a function of depth and
@@ -80,7 +80,7 @@ namespace aspect
          */
         virtual
         void
-        parse_parameters (ParameterHandler &prm);
+        parse_parameters (ParameterHandler &prm) override;
 
       private:
 
@@ -185,4 +185,4 @@ namespace aspect
 }
 
 
-#endiff
+#endif
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index 6314d989b6c..a2e327304d0 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -64,7 +64,7 @@ namespace aspect
                   ExcMessage("The initial temperature plugin lithosphere with rift requires the correspond initial composition plugin."));
 
       // Determine whether a cartesian or a spherical geometry is used.
-      cartesian_geometry = Plugins::plugin_type_matches<const GeometryModel::Box<dim>> (geometry_model);
+      cartesian_geometry = Plugins::plugin_type_matches<const GeometryModel::Box<dim>> (this->get_geometry_model());
     }
 
 
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
index 75076ace03c..2d27751e897 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -69,17 +69,17 @@ namespace aspect
       ref_rgh = 0;
       // Assume constant gravity magnitude, so ignore
       for (unsigned int l=0; l<3; ++l)
-        ref_rgh += densities[l+1] * thicknesses[l];
+        ref_rgh += densities[l+1] * reference_thicknesses[l];
 
       // The total lithosphere thickness
-      const double sum_thicknesses = std::accumulate(thicknesses.begin(), thicknesses.end(),0);
+      const double sum_thicknesses = std::accumulate(reference_thicknesses.begin(), reference_thicknesses.end(), 0);
 
       // Make sure the compensation depth is in the sublithospheric mantle
       compensation_depth = 2. * sum_thicknesses + 1e3;
 
       // The column at the rift center
       double rift_rgh = 0;
-      rift_thicknesses = thicknesses;
+      rift_thicknesses = reference_thicknesses;
       for (unsigned int l=0; l<rift_thicknesses.size(); ++l)
         rift_thicknesses[l] *= (1.-A_rift[l]);
 
@@ -148,10 +148,23 @@ namespace aspect
       for (unsigned int d=0; d<dim-1; ++d)
         surface_position[d] = position[d];
 
-      const InitialComposition::LithosphereRift<dim> &ic = initial_composition_manager->template get_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>();
+      // Get the distance to the line segments along a path parallel to the surface
+      double distance_to_rift_axis = 1e23;
+      std::pair<double,unsigned int> distance_to_L_polygon;
+      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim>>>::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
+           it != initial_composition_manager->get_active_initial_composition_conditions().end();
+           ++it)
+        if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
+          {
+            distance_to_rift_axis = ic->distance_to_rift(surface_position);
+            distance_to_L_polygon = ic->distance_to_polygon(surface_position);
+          }
 
       // Compute the topography based on distance to the rift and distance to the polygon
-      std::vector<double> local_thicknesses = ic.compute_local_thicknesses(surface_position);
+      std::vector<double> local_thicknesses(3);
+      local_thicknesses[0] = ((0.5 + 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * polygon_thicknesses[distance_to_L_polygon.second][0] + (0.5 - 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * reference_thicknesses[0]) * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0. - 2. * sigma_polygon ? 1. : (1.0 - A_rift[0] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))));
+      local_thicknesses[1] = ((0.5 + 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * polygon_thicknesses[distance_to_L_polygon.second][1] + (0.5 - 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * reference_thicknesses[1]) * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0. - 2. * sigma_polygon ? 1. : (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))));
+      local_thicknesses[2] = ((0.5 + 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * polygon_thicknesses[distance_to_L_polygon.second][2] + (0.5 - 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * reference_thicknesses[2]) * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0. - 2. * sigma_polygon ? 1. : (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))));
 
       // The local lithospheric column
       double local_rgh = 0;
@@ -187,6 +200,33 @@ namespace aspect
     void
     LithosphereRift<dim>::parse_parameters (ParameterHandler &prm)
     {
+      prm.enter_subsection ("Initial composition model");
+      {
+        prm.enter_subsection("Lithosphere with rift");
+        {
+          sigma_rift           = prm.get_double ("Standard deviation of Gaussian rift geometry");
+          sigma_polygon        = prm.get_double ("Half width of polygon smoothing");
+          blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
+          A_rift = Utilities::possibly_extend_from_1_to_N(Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
+                                                          3,
+                                                          "Amplitude of Gaussian rift geometry");
+          reference_thicknesses = Utilities::possibly_extend_from_1_to_N(Utilities::string_to_double(Utilities::split_string_list(prm.get("Layer thicknesses"))),
+                                                                         3,
+                                                                         "Layer thicknesses");
+          // Split the string into the separate polygons
+          const std::vector<std::string> temp_thicknesses = Utilities::split_string_list(prm.get("Lithospheric polygon layer thicknesses"),';');
+          const unsigned int n_polygons = temp_thicknesses.size();
+          polygon_thicknesses.resize(n_polygons);
+          for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
+            {
+              polygon_thicknesses[i_polygons] = Utilities::string_to_double(Utilities::split_string_list(temp_thicknesses[i_polygons],','));
+              AssertThrow(polygon_thicknesses[i_polygons].size()==3, ExcMessage ("The number of layer thicknesses should be equal to 3."));
+            }
+        }
+        prm.leave_subsection();
+      }
+      prm.leave_subsection();
+
       prm.enter_subsection ("Compositional fields");
       {
         list_of_composition_names = Utilities::split_string_list (prm.get("Names of fields"));
@@ -198,31 +238,12 @@ namespace aspect
         prm.enter_subsection("Visco Plastic");
         {
           n_phases_for_each_composition = std::make_unique<std::vector<unsigned int>>();
-          
-          const std::vector<unsigned int> indices = this->introspection().chemical_composition_field_indices();
-
-          std::vector<unsigned int> n_phases_for_each_chemical_composition = {n_phases_for_each_composition[0]};
-          for (auto i : indices)
-          {
-            n_phases_for_each_chemical_composition.push_back(n_phases_for_each_composition[i + 1]);
-          }
-
-          std::vector<std::string> chemical_field_names = this->introspection().chemical_composition_field_names();
-          chemical_field_names.insert(chemical_field_names.begin(), "background");
-
-          std::vector<std::string> compositional_field_names = this->introspection().get_composition_names();
-          compositional_field_names.insert(compositional_field_names.begin(), "background");
-
-          Utilities::MapParsing::Options options(chemical_field_names, "Densities");
-          options.list_of_allowed_keys = compositional_field_names;
-          options.allow_multiple_values_per_key = true;
-          options.n_values_per_key = n_phases_for_each_chemical_composition;
-          options.check_values_per_key = (options.n_values_per_key.size() != 0);
-          options.store_values_per_key = (options.n_values_per_key.size() == 0);
-
-
-          temp_densities = Utilities::MapParsing::parse_map_to_double_array (prm.get("Densities"),
-                                                                 options);
+          temp_densities = Utilities::parse_map_to_double_array (prm.get("Densities"),
+                                                                 list_of_composition_names,
+                                                                 /*has_background_field=*/true,
+                                                                 "Densities",
+                                                                 true,
+                                                                 n_phases_for_each_composition);
         }
         prm.leave_subsection();
       }
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
index 448c55e0035..bc684324522 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
@@ -46,19 +46,19 @@ namespace aspect
          * beginning of the program. Checks preconditions.
          */
         void
-        initialize ();
+        initialize () override;
 
         /**
          * Return the value of the topography for a point.
          */
         virtual
-        double value (const Point<dim-1> &p) const;
+        double value (const Point<dim-1> &p) const override;
 
         /**
          * Return the maximum value of the elevation.
          */
         virtual
-        double max_topography () const;
+        double max_topography () const override;
 
         /**
          * Declare the parameters this class takes through input files.
@@ -72,7 +72,7 @@ namespace aspect
          */
         virtual
         void
-        parse_parameters (ParameterHandler &prm);
+        parse_parameters (ParameterHandler &prm) override;
 
       private:
         /**
diff --git a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
index d8bdd7329af..831dc9ab86e 100644
--- a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
+++ b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.h
@@ -53,7 +53,7 @@ namespace aspect
          * Initialization function.
          */
         void
-        initialize ();
+        initialize () override;
 
         /**
          * Return the initial composition as a function of position and number
@@ -61,7 +61,7 @@ namespace aspect
          * around a user-defined set of line-segments.
          */
         virtual
-        double initial_composition (const Point<dim> &position, const unsigned int n_comp) const;
+        double initial_composition (const Point<dim> &position, const unsigned int n_comp) const override;
 
         /**
          * Declare the parameters this class takes through input files. The
@@ -81,7 +81,7 @@ namespace aspect
          */
         virtual
         void
-        parse_parameters (ParameterHandler &prm);
+        parse_parameters(ParameterHandler &prm) override;
 
       private:
 

From 51694d54efe778142c00f7ec80eda9ca2c5f4976 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 30 May 2024 19:26:19 +0200
Subject: [PATCH 23/38] Update prm

---
 .../initial_conditions_continental_rift.prm   | 211 +++++++-----------
 1 file changed, 86 insertions(+), 125 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
index 4ef594afbaa..186ed221b5a 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
@@ -1,31 +1,19 @@
-#### Continental Extension Cookbook
-# This cookbook is based off numerous published studies, five of which are listed below.
-# For additional information, see these publications and references therein.
-#   1. Brune, S., Heine, C., Perez-Gussinye, M., and Sobolev, S.V. (2014), Nat. Comm., v.5, n.4014,
-#      Rift migration explains continental margin asymmetry and crustal hyperextension
-#   2. Huismans, R., and Beaumont, C. (2011), Nature, v.473, p.71-75.
-#      Depth-dependent extension, two-stage breakup and cratonic underplating at rifted margins
-#   3. Naliboff, J., and Buiter, S.H. (2015), Earth Planet. Sci. Lett., v.421, p.58-67,
-#      "Rift Reactivation and migration during multiphase extension"
-#   4. Naliboff, J., Glerum, A., Sascha, S., Peron-Pinvidic, G., and Wrona, T. (2020), Geophys.
-#      Res. Lett., 47, e2019GL086611, "Development of 3‐D rift heterogeneity through fault
-#      network evolution"
-#   5. Sandiford, D., Brune, S., Glerum, A., Naliboff, J., and Whittaker, J.M. (2021), Geophys.
-#      Geochem. Geosys., 22, e2021GC009681, "Kinematics of footwall exhumation at oceanic
-#      detachment faults: Solid-block rotation and apparent unbending"
+#### This is an adaptation of the Continental Extension Cookbook
+#### using new plugins for the initial composition, temperature
+#### topography and strain of an incipient continental rift system.
 
 ####  Global parameters
-set Additional shared libraries            = /Applications/ASPECT/VisualStudioCode/aspect/cookbooks/initial_conditions_continental_rift/libinitial_conditions_continental_rift.debug.so
+set Additional shared libraries            = $ASPECT_SOURCE_DIR/cookbooks/initial_conditions_continental_rift/libinitial_conditions_continental_rift.debug.so
 set Dimension                              = 2
 set Start time                             = 0
-set End time                               = 5e6
+set End time                               = 0 #5e6
 set Use years in output instead of seconds = true
-set Nonlinear solver scheme                = single Advection, iterated defect correction Stokes
-set Nonlinear solver tolerance             = 1e-4
+set Nonlinear solver scheme                = single Advection, iterated Stokes
+set Nonlinear solver tolerance             = 1e-5
 set Max nonlinear iterations               = 2
 set CFL number                             = 0.5
 set Maximum time step                      = 20e3
-set Output directory                       = output-continental_extension
+set Output directory                       = output-initial_conditions_continental_rift
 set Pressure normalization                 = no
 
 #### Parameters describing the model
@@ -65,20 +53,11 @@ subsection Mesh refinement
   end
 end
 
-# Use the Eisenstat Walker method to automatically determine the
-# linear solver tolerance during the defect Picard iterations.
-# Adjusting the Maximum linear solver tolerance will affect how long
-# it takes to reach a solution, but not the actual value of the
-# solution.
+
 subsection Solver parameters
   subsection Stokes solver parameters
     set Number of cheap Stokes solver steps = 0
   end
-
-  subsection Newton solver parameters
-    set Maximum linear Stokes solver tolerance   = 1e-2
-    set Use Eisenstat Walker method for Picard iterations = true
-  end
 end
 
 # Advecting the free surface using a normal, rather than vertical,
@@ -128,58 +107,69 @@ subsection Compositional fields
 end
 
 # Initial values of different compositional fields
-# The upper crust (20 km thick), lower crust (20 km thick)
-# and mantle (60 km thick) are continuous horizontal layers
-# of constant thickness. The non initial plastic strain is set
+# The upper crust (20 km thick), lower crust (15 km thick)
+# and mantle (85 km thick) are continuous horizontal layers
+# of constant thickness, except in a center area.
+# In the centre of the domain, the upper crust is thickened to 25 km,
+# while the mantle lithosphere is thinned. The transition from this
+# perturbed center to the reference thicknesses of the lithospheric
+# layers is smoothened using a Gaussian. The combined effect
+# is a hotter, weaker centre area that localizes deformation.
+# An additional thicker/stronger area is added on the right of the domain
+# to represent cratonic lithosphere. The transition in layer thicknesses
+# uses a hyperbolic tangent.
+# The non initial plastic strain is set
 # to 0 and the initial plastic strain is randomized between
-# 0.5 and 1.5.
+# 0.5 and 1.5 in an area around the rift axis.
 subsection Initial composition model
   set List of model names = lithosphere with rift, rift box initial plastic strain, function
 
   subsection Lithosphere with rift
-    set Blend polygons and rifts                       = true
-    set Standard deviation of Gaussian rift geometry   = 60e3
-    set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
-    # LAB at 110 km
-    set Rift axis line segments                        = 350e3
+    # The reference layer thicknesses of the upper crust, lower crust and mantle lithosphere.
     set Layer thicknesses                              = 20e3, 15e3, 85e3
-
-    # Polygon LAB at 200 km
-    set Lithospheric polygon layer thicknesses         = 23e3, 20e3 , 157.e3
-    set Lithospheric polygons                          = 450e3 > 3000e3
+    # How wide the weak zone will be
+    set Standard deviation of Gaussian rift geometry   = 50e3
+    # The maximum thinning/thickening of the lithospheric layers
+    set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
+    # Where the rift axis should be. In this case in the centre of the domain.
+    # In 3D simulations, line segments consisting of two coordinates
+    # should be provided. 
+    set Rift axis line segments                        = 100e3
+
+    # The thicknesses of the lithospheric layer within a polygon
+    set Lithospheric polygon layer thicknesses         = 20e3, 15e3 , 115.e3
+    # The segments making up the polygon
+    set Lithospheric polygons                          = 150e3 > 3000e3
+    # The half width of the transition from polygon to reference lithosphere
     set Half width of polygon smoothing                = 10e3
   end
 
-  # Inherited noise
+  # Inherited plastic strain
   subsection Rift box initial plastic strain
-    set Standard deviation of Gaussian noise amplitude distribution   = 200e3
+    # We focus initial strain around the rift axis
+    set Rift axis line segments                                         = 100e3
+    # The strain values follow a Gaussian distribution around the rift axis
+    # The maximum magnitude of the strain
     set Maximum amplitude of Gaussian noise amplitude distribution      = 0.250000
+    # The sigma width of the area of strain
+    set Standard deviation of Gaussian noise amplitude distribution     = 50e3
+    # The number with which to start of the random number generator
     set Random number generator seed                                    = 2.000000
+    # Using a hyperbolic tangent centred around this value,
+    # we smooth out the strain with increasing depth.
     set Depth around which Gaussian noise is smoothed out               = 50e3
+    # The halfwidth of the hyperbolic tangent.
     set Halfwidth with which Gaussian noise is smoothed out in depth    = 10e3
-    #set Grid intervals for noise X or radius                            = 2240
-    # Add 16 intervals for the additional 5 km that is added to the grid
-    # to account for initial topography
-    #set Grid intervals for noise Y or longitude                         = 976 #960
-    set Rift axis line segments                                         = 350e3
   end
 
   subsection Function
     set Variable names = x,y
-    set Function expression           = 0; \
-                                        0; \
-                                        0; \
-          0; \
-          0
+    set Function expression = 0; \
+                              0; \
+                              0; \
+                              0; \
+                              0
   end
-#  subsection Function
-#    set Variable names      = x,y
-#    set Function expression = 0; \
-#                              if(x>50.e3 && x<150.e3 && y>50.e3, 0.5 + rand_seed(1), 0); \
-#                              if(y>=80.e3, 1, 0); \
-#                              if(y<80.e3 && y>=60.e3, 1, 0); \
-#                              if(y<60.e3, 1, 0);
-#  end
 end
 
 # Composition: fixed on bottom (inflow boundary), free on sides and top
@@ -187,50 +177,38 @@ subsection Boundary composition model
   set Fixed composition boundary indicators = bottom
   set List of model names = function
   subsection Function
-    set Function expression           = 0; \
-                                        0; \
-                                        0; \
-          0; \
-          0
+    set Function expression = 0; \
+                              0; \
+                              0; \
+                              0; \
+                              0
   end
 end
 
 # Temperature boundary conditions
-# Top and bottom (fixed) temperatures are consistent with the initial temperature field
-# Note that while temperatures are specified for the model sides, these values are
-# not used as the sides are not specified "Fixed temperature boundaries".  Rather,
-# these boundaries are insulating (zero net heat flux).
+# Top and bottom (fixed) temperatures are consistent with the initial temperature field.
+# Because we use a free surface, the height/depth of the surface can change over time,
+# meaning that if the initial temperature plugin is asked for the temperature
+# at the surface, this temperature could also vary over time. Therefore
+# we also use the box plugin and take the minimum of the initial temperature and
+# the box plugins, thus maintaining a temperature of 293 K.
 subsection Boundary temperature model
-  set Fixed temperature boundary indicators = bottom, top
-  set List of model names = box
-
+  set Fixed temperature boundary indicators   = bottom, top
+  set List of model names = initial temperature, box
+  set List of model operators = add, minimum
   subsection Box
-    set Bottom temperature = 1613
-    set Top temperature    =  273
+    set Top temperature    =  293
+    # Unrealistically high, so that it is always taken from initial temperature plugin
+    set Bottom temperature = 5000   
   end
 end
 
 # Initial temperature field
-# Typical continental geotherm based on equations 4-6 from:
-#   D.S. Chapman (1986), "Thermal gradients in the continental crust",
-#   Geological Society of London Special Publications, v.24, p.63-70.
-# The initial constraints are:
-#   Surface Temperature  - upper crust (ts1) = 273 K
-#   Surface Heat Flow    - upper crust (qs1) = 0.055 mW/m^2
-#   Heat Production      - upper crust (A1)  = 1.00e-6 W/m^3;
-#   Heat Production      - lower crust (A2)  = 0.25e-6 W/m^3;
-#   Heat Production      - mantle (A3)       = 0.00e-6 W/m^3;
-#   Thermal Conductivity - all layers        = 2.5 (W/(m K));
-# To satisfy these constraints, the following values are required:
-#   Surface Temperature  - lower crust (ts2) = 633 K
-#                        - mantle (ts3)      = 893 K
-#   Surface Heat Flow    - lower crust (qs2) = 0.035 W/m^2;
-#                        - mantle      (qs3) = 0.030 W/m^2;
-# Note: The continental geotherm initial temperature model
-#       plugin can be used to compute an identical geotherm
-#       for the lithosphere. An example of how to use this
-#       plugin is illustrated in the test for this cookbook
-#       (tests/continental_extension.prm).
+# The initial temperature consists of a typical continental geotherm
+# based on equations Turcotte and Schubert Ch. 4.6.
+# Below the lithosphere-asthenosphere boundary (LAB, defined initially by the 
+# bottom of the mantle lithsphere and the 1623 K isotherm,
+# we prescribe an adiabatic temperature increase.
 subsection Initial temperature model
   set List of model names = adiabatic, lithosphere with rift
   set List of model operators = add, replace if valid
@@ -238,8 +216,7 @@ subsection Initial temperature model
     set LAB isotherm temperature = 1623.
     set Surface temperature = 293.
     # Whether or not to prescribe the LAB depth up to a
-    # certain depth (in area below LAB)
-    # or use adiabat everywhere
+    # certain depth (in area below LAB) or use the adiabat everywhere, 
     set Use temperature compensation depth = true
     set Temperature compensation depth = 200e3
   end
@@ -247,34 +224,18 @@ subsection Initial temperature model
     # A reference profile of the compositional fields
     # where x represents depth
     subsection Function
-    #  plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio_marine_continental_sediment, silt_fraction
-       set Function expression           = 0; \
-                                           0; \
-                                           0; \
-                                           0; \
-             0; \
-                                           if(x<23e3,1,0); \
-                                           if(x>=23e3&x<43e3,1,0); \
-                                           if(x>=43e3&x<200e3,1,0); \
-                                           0; \
-                                           0
+    # noninitial_plastic_strain, plastic_strain, upper, lower, mantle_L
+    set Function expression           = 0; \
+                                        0; \
+                                        if(x<20e3,1,0); \
+                                        if(x>=20e3&x<35e3,1,0); \
+                                        if(x>=35e3&x<120e3,1,0); \
     end
+    # No thermal boundary layers, as we already add a continental geotherm
     set Age top boundary layer        = 0
     set Age bottom boundary layer     = 0
   end
 
-  subsection Function
-    set Variable names = x,y
-    set Function constants = h=100e3, ts1=273, ts2=633, ts3=893, \
-                             A1=1.e-6, A2=0.25e-6, A3=0.0, \
-                             k1=2.5, k2=2.5, k3=2.5, \
-                             qs1=0.055, qs2=0.035, qs3=0.030
-    set Function expression = if( (h-y)<=20.e3, \
-                                  ts1 + (qs1/k1)*(h-y) - (A1*(h-y)*(h-y))/(2.0*k1), \
-                                  if( (h-y)>20.e3 && (h-y)<=40.e3, \
-                                      ts2 + (qs2/k2)*(h-y-20.e3) - (A2*(h-y-20.e3)*(h-y-20.e3))/(2.0*k2), \
-                                      ts3 + (qs3/k3)*(h-y-40.e3) - (A3*(h-y-40.e3)*(h-y-40.e3))/(2.0*k3) ) );
-  end
 end
 
 # Constant internal heat production values (W/m^3) for background material
@@ -283,7 +244,7 @@ subsection Heating model
   set List of model names = compositional heating
 
   subsection Compositional heating
-    set Use compositional field for heat production averaging = 1, 0, 0, 1, 1, 1
+    set Use compositional field for heat production averaging = 0, 0, 1, 1, 1
     set Compositional heating values = 0.0, 0.0, 0.0, 1.0e-6, 0.25e-6, 0.
   end
 end
@@ -376,10 +337,10 @@ end
 
 # Post processing
 subsection Postprocess
-  set List of postprocessors = composition statistics, heat flux densities, heat flux statistics, mass flux statistics, pressure statistics, temperature statistics, topography, velocity statistics, visualization
+  set List of postprocessors = composition statistics, temperature statistics, topography, velocity statistics, visualization
 
   subsection Visualization
-    set List of output variables = density, heat flux map, named additional outputs, strain rate, viscosity
+    set List of output variables = density, named additional outputs, strain rate, viscosity
     set Output format                 = vtu
     set Time between graphical output = 100.e3
     set Interpolate output            = true

From 7933e9b95375dda4c745a8be7fe876aedc7d4c15 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 30 May 2024 22:29:29 +0200
Subject: [PATCH 24/38] Fix IC and IT

---
 ...continental_rift_no_initial_topography.prm | 342 ++++++++++++++++++
 .../lithosphere_rift_IC.cc                    |   5 +-
 .../lithosphere_rift_IT_2.cc                  |   8 +-
 3 files changed, 352 insertions(+), 3 deletions(-)
 create mode 100644 cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm

diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
new file mode 100644
index 00000000000..56fc5a19662
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
@@ -0,0 +1,342 @@
+#### This is an adaptation of the Continental Extension Cookbook
+#### using new plugins for the initial composition, temperature
+#### topography and strain of an incipient continental rift system.
+
+####  Global parameters
+set Additional shared libraries            = $ASPECT_SOURCE_DIR/cookbooks/initial_conditions_continental_rift/libinitial_conditions_continental_rift.debug.so
+set Dimension                              = 2
+set Start time                             = 0
+set End time                               = 0 #5e6
+set Use years in output instead of seconds = true
+set Nonlinear solver scheme                = single Advection, iterated Stokes
+set Nonlinear solver tolerance             = 1e-5
+set Max nonlinear iterations               = 2
+set CFL number                             = 0.5
+set Maximum time step                      = 20e3
+set Output directory                       = output-initial_conditions_continental_rift_no_initial_topography
+set Pressure normalization                 = no
+set Adiabatic surface temperature          = 1573
+
+#### Parameters describing the model
+
+# Governing equations
+subsection Formulation
+  set Formulation = Boussinesq approximation
+end
+
+# Model geometry (400x200 km, 40 km spacing)
+subsection Geometry model
+  set Model name = box
+
+  subsection Box
+    set X repetitions = 10
+    set Y repetitions = 5
+    set X extent      = 400e3
+    set Y extent      = 200e3
+  end
+end
+
+# Globally refine the mesh to 2.5 km spacing, and then
+# adaptively refine the mesh to 1.25 km spacing above y=50 km
+# and between x=40 and x=160 km. These values ensure areas
+# undergoing brittle deformation are in the high-resolution
+# region.
+subsection Mesh refinement
+  set Initial adaptive refinement        = 0
+  set Initial global refinement          = 3
+  set Time steps between mesh refinement = 0
+  set Strategy = minimum refinement function
+
+  subsection Minimum refinement function
+    set Coordinate system   = cartesian
+    set Variable names      = x,y
+    set Function expression = if ( y>=50e3 && x>=40.e3 && x<=160.e3, 4, 3)
+  end
+end
+
+
+subsection Solver parameters
+  subsection Stokes solver parameters
+    set Number of cheap Stokes solver steps = 0
+  end
+end
+
+# Advecting the free surface using a normal, rather than vertical,
+# projection. To reduce mesh instabilities and associated solver
+# issues when deformation becomes large, diffusion is applied to
+# the free surface at each time step.
+subsection Mesh deformation
+  set Mesh deformation boundary indicators        = top: free surface, top: diffusion
+
+  subsection Free surface
+    set Surface velocity projection = normal
+  end
+
+  subsection Diffusion
+    # Diffusivity term. Increasing this value will result
+    # in a smoother free surface and lower topography
+    # amplitudes.
+    set Hillslope transport coefficient = 1.e-8
+  end
+end
+
+# Velocity on boundaries characterized by functions
+# The outward velocity (x-direction) on the left and right walls is 0.25 cm/year
+# The vertical velocity at the base is 0.25 cm/year (balances outflow on sides)
+# Velocity components parallel to the base (x-velocity) and side walls (y-velocity)
+# are unconstrained (i.e. 'free').
+subsection Boundary velocity model
+  set Prescribed velocity boundary indicators = left x: function, right x:function, bottom y:function
+
+  subsection Function
+    set Variable names      = x,y
+    set Function constants  = v=0.0025, w=200.e3, d=100.e3
+    set Function expression = if (x < w/2 , -v, v) ; v*2*d/w
+  end
+end
+
+# Number and names of compositional fields
+# The five compositional fields represent:
+# 1. The plastic strain that accumualates over time, with the initial plastic strain removed
+# 2. The plastic strain that accumulated over time, including the initial plastic strain values
+# 3. The upper crust
+# 4. The lower crust
+# 5. The mantle lithosphere
+subsection Compositional fields
+  set Number of fields = 5
+  set Names of fields = noninitial_plastic_strain, plastic_strain, upper, lower, mantle_L
+end
+
+# Initial values of different compositional fields
+# The upper crust (20 km thick), lower crust (15 km thick)
+# and mantle (85 km thick) are continuous horizontal layers
+# of constant thickness, except in a center area.
+# In the centre of the domain, the upper crust is thickened to 25 km,
+# while the mantle lithosphere is thinned. The transition from this
+# perturbed center to the reference thicknesses of the lithospheric
+# layers is smoothened using a Gaussian. The combined effect
+# is a hotter, weaker centre area that localizes deformation.
+# An additional thicker/stronger area is added on the right of the domain
+# to represent cratonic lithosphere. The transition in layer thicknesses
+# uses a hyperbolic tangent.
+# The non initial plastic strain is set
+# to 0 and the initial plastic strain is randomized between
+# 0.5 and 1.5 in an area around the rift axis.
+subsection Initial composition model
+  set List of model names = lithosphere with rift, rift box initial plastic strain, function
+
+  subsection Lithosphere with rift
+    # The reference layer thicknesses of the upper crust, lower crust and mantle lithosphere.
+    set Layer thicknesses                              = 20e3, 15e3, 85e3
+    # How wide the weak zone will be
+    set Standard deviation of Gaussian rift geometry   = 50e3
+    # The maximum thinning/thickening of the lithospheric layers
+    set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
+    # Where the rift axis should be. In this case in the centre of the domain.
+    # In 3D simulations, line segments consisting of two coordinates
+    # should be provided. 
+    set Rift axis line segments                        = 200e3
+
+    # The thicknesses of the lithospheric layer within a polygon
+    set Lithospheric polygon layer thicknesses         = 20e3, 15e3 , 115.e3
+    # The segments making up the polygon
+    set Lithospheric polygons                          = 550e3 > 3000e3
+    # The half width of the transition from polygon to reference lithosphere
+    set Half width of polygon smoothing                = 10e3
+  end
+
+  # Inherited plastic strain
+  subsection Rift box initial plastic strain
+    # We focus initial strain around the rift axis
+    set Rift axis line segments                                         = 200e3
+    # The strain values follow a Gaussian distribution around the rift axis
+    # The maximum magnitude of the strain
+    set Maximum amplitude of Gaussian noise amplitude distribution      = 0.250000
+    # The sigma width of the area of strain
+    set Standard deviation of Gaussian noise amplitude distribution     = 50e3
+    # The number with which to start of the random number generator
+    set Random number generator seed                                    = 2
+    # Using a hyperbolic tangent centred around this value,
+    # we smooth out the strain with increasing depth.
+    set Depth around which Gaussian noise is smoothed out               = 50e3
+    # The halfwidth of the hyperbolic tangent.
+    set Halfwidth with which Gaussian noise is smoothed out in depth    = 10e3
+  end
+
+  subsection Function
+    set Variable names = x,y
+    set Function expression = 0; \
+                              0; \
+                              0; \
+                              0; \
+                              0
+  end
+end
+
+# Composition: fixed on bottom (inflow boundary), free on sides and top
+subsection Boundary composition model
+  set Fixed composition boundary indicators = bottom
+  set List of model names = function
+  subsection Function
+    set Function expression = 0; \
+                              0; \
+                              0; \
+                              0; \
+                              0
+  end
+end
+
+# Temperature boundary conditions
+# Top and bottom (fixed) temperatures are consistent with the initial temperature field.
+# Because we use a free surface, the height/depth of the surface can change over time,
+# meaning that if the initial temperature plugin is asked for the temperature
+# at the surface, this temperature could also vary over time. Therefore
+# we also use the box plugin and take the minimum of the initial temperature and
+# the box plugins, thus maintaining a temperature of 293 K.
+subsection Boundary temperature model
+  set Fixed temperature boundary indicators   = bottom, top
+  set List of model names = initial temperature, box
+  set List of model operators = add, minimum
+  subsection Box
+    set Top temperature    =  293
+    # Unrealistically high, so that it is always taken from initial temperature plugin
+    set Bottom temperature = 5000   
+  end
+end
+
+# Initial temperature field
+# The initial temperature consists of a typical continental geotherm
+# based on equations Turcotte and Schubert Ch. 4.6.
+# Below the lithosphere-asthenosphere boundary (LAB, defined initially by the 
+# bottom of the mantle lithsphere and the 1623 K isotherm,
+# we prescribe an adiabatic temperature increase.
+subsection Initial temperature model
+  set List of model names = adiabatic, lithosphere with rift
+  set List of model operators = add, replace if valid
+  subsection Lithosphere with rift
+    set LAB isotherm temperature = 1573.
+    set Surface temperature = 293.
+  end
+  subsection Adiabatic
+    # A reference profile of the compositional fields
+    # where x represents depth
+    subsection Function
+    # noninitial_plastic_strain, plastic_strain, upper, lower, mantle_L
+    set Function expression           = 0; \
+                                        0; \
+                                        if(x<20e3,1,0); \
+                                        if(x>=20e3&x<35e3,1,0); \
+                                        if(x>=35e3&x<120e3,1,0)
+    end
+  end
+
+end
+
+# Constant internal heat production values (W/m^3) for background material
+# and compositional fields.
+subsection Heating model
+  set List of model names = compositional heating
+
+  subsection Compositional heating
+    set Use compositional field for heat production averaging = 0, 0, 0, 1, 1, 1
+    set Compositional heating values = 0.0, 0.0, 0.0, 1.0e-6, 0.25e-6, 0.
+  end
+end
+
+# Material model
+# Rheology: Non-linear viscous flow and Drucker Prager Plasticity
+# Values for most rheological parameters are specified for a background material and
+# each compositional field.  Values for viscous deformation are based on dislocation
+# creep flow-laws, with distinct values for the upper crust (wet quartzite), lower
+# crust (wet anorthite) and mantle (dry olivine).  Table 1 of Naliboff and Buiter (2015),
+# Earth Planet. Sci. Lett., v.421, p. 58-67 contains values for each of these flow laws.
+subsection Material model
+  set Model name = visco plastic
+
+  subsection Visco Plastic
+    # Reference temperature and viscosity
+    set Reference temperature = 273
+
+    # The minimum strain-rate helps limit large viscosities values that arise
+    # as the strain-rate approaches zero.
+    # The reference strain-rate is used on the first non-linear iteration
+    # of the first time step when the velocity has not been determined yet.
+    set Minimum strain rate = 1.e-20
+    set Reference strain rate = 1.e-16
+
+    # Limit the viscosity with minimum and maximum values
+    set Minimum viscosity = 1e18
+    set Maximum viscosity = 1e26
+
+    # Thermal diffusivity is adjusted to match thermal conductivities
+    # assumed in assigning the initial geotherm
+    set Define thermal conductivities = true
+    set Thermal conductivities        = 2.5
+    set Heat capacities               = 750.
+
+    # Density values of 1 are assigned to "strain" fields, which are not taken into
+    # account when computing material properties.
+    set Densities                     = 3300, 1.0, 1.0, 2700,  2900, 3300
+    set Thermal expansivities         = 2e-5
+
+    # Harmonic viscosity averaging
+    set Viscosity averaging scheme = harmonic
+
+    # Choose to have the viscosity (pre-yield) follow a dislocation
+    # diffusion or composite flow law.  Here, dislocation is selected
+    # so no need to specify diffusion creep parameters below, which are
+    # only used if "diffusion" or "composite" option is selected.
+    set Viscous flow law = dislocation
+
+    # Dislocation creep parameters for
+    # 1. Background material/mantle (dry olivine)
+    #    Hirth & Kohlstedt (2004),  Geophys. Monogr. Am. Geophys. Soc., v.138, p.83-105.
+    #    "Rheology of the upper mantle and the mantle wedge:a view from the experimentalists"
+    # 2. Upper crust (wet quartzite)
+    #    Rutter & Brodie (2004), J. Struct. Geol., v.26, p.2011-2023.
+    #    "Experimental grain size-sensitive flow of hot-pressed Brazilian quartz aggregates"
+    # 3. Lower crust and weak seed (wet anorthite)
+    #    Rybacki et al. (2006), J. Geophys. Res., v.111(B3).
+    #    "Influence of water fugacity and activation volume on the flow properties of fine-grained
+    #    anorthite aggregates"
+    # Note that the viscous pre-factors below are scaled to plane strain from unixial strain experiments.
+    # For ease of identification, fields tracking strain are assigned prefactors of 1e-50
+    set Prefactors for dislocation creep          = 6.52e-16, 1.00e-50, 1.00e-50, 8.57e-28, 7.13e-18, 6.52e-16
+    set Stress exponents for dislocation creep    =      3.5,      1.0,      1.0,      4.0,      3.0,      3.5
+    set Activation energies for dislocation creep =   530.e3,      0.0,      0.0,   223.e3,   345.e3,   530.e3
+    set Activation volumes for dislocation creep  =   18.e-6,      0.0,      0.0,      0.0,      0.0,   18.e-6
+
+    # Plasticity parameters
+    set Angles of internal friction = 30
+    set Cohesions                   = 20.e6
+
+    # The parameters below weaken the friction and cohesion by a
+    # a factor of 4 between plastic strain values of 0.5 and 1.5.
+    set Strain weakening mechanism                   = plastic weakening with plastic strain only
+    set Start plasticity strain weakening intervals  = 0.5
+    set End plasticity strain weakening intervals    = 1.5
+    set Cohesion strain weakening factors            = 0.25
+    set Friction strain weakening factors            = 0.25
+  end
+end
+
+# Gravity model
+subsection Gravity model
+  set Model name = vertical
+
+  subsection Vertical
+    set Magnitude = 9.81
+  end
+end
+
+# Post processing
+subsection Postprocess
+  set List of postprocessors = composition statistics, temperature statistics, topography, velocity statistics, visualization
+
+  subsection Visualization
+    set List of output variables = density, named additional outputs, strain rate, viscosity
+    set Output format                 = vtu
+    set Time between graphical output = 100.e3
+    set Interpolate output            = true
+  end
+end
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
index 5f667e72e62..38be60fe572 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
@@ -71,7 +71,7 @@ namespace aspect
       else if (depth > local_thicknesses[0] && depth <= local_thicknesses[0] + local_thicknesses[1]
                && compositional_index == id_lower)
         return 1.;
-      else if (depth > local_thicknesses[0] + local_thicknesses[2] && depth <= local_thicknesses[0] + local_thicknesses[1] + local_thicknesses[2]
+      else if (depth > local_thicknesses[0] + local_thicknesses[1] && depth <= local_thicknesses[0] + local_thicknesses[1] + local_thicknesses[2]
                && compositional_index == id_mantle_L)
         return 1.;
       else
@@ -174,9 +174,12 @@ namespace aspect
 
       // Compute the local thickness of the upper crust, lower crust and mantle part of the lithosphere
       // (in this exact order) based on the distance from the rift axis and the polygons.
+      // The transition from reference and/or rift perturbation lithosphere to polygon lithosphere
+      // is smoothed by a hyperbolic tangent.
       const double polygon_contribution = (0.5 + 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon));
       const double rift_contribution = (0.5 - 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon));
       
+      // The rift perturbation follows a Gaussian contribution.
       std::vector<double> local_thicknesses(3);
       for (unsigned int i = 0; i < 3; ++i)
         local_thicknesses[i] = (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))) 
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index a2e327304d0..dc644ac9a6d 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -60,8 +60,9 @@ namespace aspect
         initial_composition_manager = this->get_initial_composition_manager_pointer();
 
       // Check that the required initial composition model is used.
-      AssertThrow(initial_composition_manager->template has_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>(),
-                  ExcMessage("The initial temperature plugin lithosphere with rift requires the correspond initial composition plugin."));
+      // This doesn't work during initialization.
+      //AssertThrow(initial_composition_manager->template has_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>(),
+      //             ExcMessage("The initial temperature plugin lithosphere with rift requires the corresponding initial composition plugin."));
 
       // Determine whether a cartesian or a spherical geometry is used.
       cartesian_geometry = Plugins::plugin_type_matches<const GeometryModel::Box<dim>> (this->get_geometry_model());
@@ -73,6 +74,9 @@ namespace aspect
     LithosphereRift<dim>::
     initial_temperature (const Point<dim> &position) const
     {
+      Assert(initial_composition_manager->template has_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>(),
+                  ExcMessage("The initial temperature plugin lithosphere with rift requires the corresponding initial composition plugin."));
+                  
       // Get the initial composition plugin
       const InitialComposition::LithosphereRift<dim> &ic = initial_composition_manager->template get_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>();
 

From c2bf6d281810c91245a81857f28919db10cbf526 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 30 May 2024 22:31:11 +0200
Subject: [PATCH 25/38] Rename prm

---
 ...s_continental_rift_initial_topography.prm} | 38 ++++++++++---------
 1 file changed, 20 insertions(+), 18 deletions(-)
 rename cookbooks/initial_conditions_continental_rift/{initial_conditions_continental_rift.prm => initial_conditions_continental_rift_initial_topography.prm} (94%)

diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
similarity index 94%
rename from cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
rename to cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
index 186ed221b5a..5621f14a757 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
@@ -13,8 +13,9 @@ set Nonlinear solver tolerance             = 1e-5
 set Max nonlinear iterations               = 2
 set CFL number                             = 0.5
 set Maximum time step                      = 20e3
-set Output directory                       = output-initial_conditions_continental_rift
+set Output directory                       = output-initial_conditions_continental_rift_initial_topography
 set Pressure normalization                 = no
+set Adiabatic surface temperature          = 1573
 
 #### Parameters describing the model
 
@@ -23,16 +24,24 @@ subsection Formulation
   set Formulation = Boussinesq approximation
 end
 
-# Model geometry (200x100 km, 20 km spacing)
+# Model geometry (400x200 km, 40 km spacing)
 subsection Geometry model
   set Model name = box
 
   subsection Box
     set X repetitions = 10
     set Y repetitions = 5
-    set X extent      = 200e3
-    set Y extent      = 100e3
+    set X extent      = 400e3
+    set Y extent      = 200e3
   end
+
+  # With respect to the reference lithosphere,
+  # move the surface of perturbed lithosphere
+  # to obtain isostasy.
+  subsection Initial topography model
+    set Model name = lithosphere with rift
+  end 
+
 end
 
 # Globally refine the mesh to 2.5 km spacing, and then
@@ -134,12 +143,12 @@ subsection Initial composition model
     # Where the rift axis should be. In this case in the centre of the domain.
     # In 3D simulations, line segments consisting of two coordinates
     # should be provided. 
-    set Rift axis line segments                        = 100e3
+    set Rift axis line segments                        = 200e3
 
     # The thicknesses of the lithospheric layer within a polygon
     set Lithospheric polygon layer thicknesses         = 20e3, 15e3 , 115.e3
     # The segments making up the polygon
-    set Lithospheric polygons                          = 150e3 > 3000e3
+    set Lithospheric polygons                          = 550e3 > 3000e3
     # The half width of the transition from polygon to reference lithosphere
     set Half width of polygon smoothing                = 10e3
   end
@@ -147,14 +156,14 @@ subsection Initial composition model
   # Inherited plastic strain
   subsection Rift box initial plastic strain
     # We focus initial strain around the rift axis
-    set Rift axis line segments                                         = 100e3
+    set Rift axis line segments                                         = 200e3
     # The strain values follow a Gaussian distribution around the rift axis
     # The maximum magnitude of the strain
     set Maximum amplitude of Gaussian noise amplitude distribution      = 0.250000
     # The sigma width of the area of strain
     set Standard deviation of Gaussian noise amplitude distribution     = 50e3
     # The number with which to start of the random number generator
-    set Random number generator seed                                    = 2.000000
+    set Random number generator seed                                    = 2
     # Using a hyperbolic tangent centred around this value,
     # we smooth out the strain with increasing depth.
     set Depth around which Gaussian noise is smoothed out               = 50e3
@@ -213,12 +222,8 @@ subsection Initial temperature model
   set List of model names = adiabatic, lithosphere with rift
   set List of model operators = add, replace if valid
   subsection Lithosphere with rift
-    set LAB isotherm temperature = 1623.
+    set LAB isotherm temperature = 1573.
     set Surface temperature = 293.
-    # Whether or not to prescribe the LAB depth up to a
-    # certain depth (in area below LAB) or use the adiabat everywhere, 
-    set Use temperature compensation depth = true
-    set Temperature compensation depth = 200e3
   end
   subsection Adiabatic
     # A reference profile of the compositional fields
@@ -229,11 +234,8 @@ subsection Initial temperature model
                                         0; \
                                         if(x<20e3,1,0); \
                                         if(x>=20e3&x<35e3,1,0); \
-                                        if(x>=35e3&x<120e3,1,0); \
+                                        if(x>=35e3&x<120e3,1,0)
     end
-    # No thermal boundary layers, as we already add a continental geotherm
-    set Age top boundary layer        = 0
-    set Age bottom boundary layer     = 0
   end
 
 end
@@ -244,7 +246,7 @@ subsection Heating model
   set List of model names = compositional heating
 
   subsection Compositional heating
-    set Use compositional field for heat production averaging = 0, 0, 1, 1, 1
+    set Use compositional field for heat production averaging = 0, 0, 0, 1, 1, 1
     set Compositional heating values = 0.0, 0.0, 0.0, 1.0e-6, 0.25e-6, 0.
   end
 end

From 59f13d7b43afce0a41fa2d6490a82d54a21303c6 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 31 May 2024 01:34:21 +0200
Subject: [PATCH 26/38] Update text with figure

---
 .../doc/Initial_density_with_craton.png       | Bin 0 -> 35944 bytes
 .../Initial_plastic_strain_with_craton.png    | Bin 0 -> 269998 bytes
 .../doc/Initial_temperature_with_craton.png   | Bin 0 -> 99953 bytes
 .../doc/Initial_topography_with_craton.png    | Bin 0 -> 195918 bytes
 .../doc/lithosphere_with_rift_IC_cookbook.md  | 109 ++++++++++++++++++
 5 files changed, 109 insertions(+)
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/Initial_density_with_craton.png
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/Initial_plastic_strain_with_craton.png
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/Initial_temperature_with_craton.png
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/Initial_topography_with_craton.png
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md

diff --git a/cookbooks/initial_conditions_continental_rift/doc/Initial_density_with_craton.png b/cookbooks/initial_conditions_continental_rift/doc/Initial_density_with_craton.png
new file mode 100644
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diff --git a/cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md b/cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md
new file mode 100644
index 00000000000..e92a6e347c7
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md
@@ -0,0 +1,109 @@
+# Initial conditions for continental rifting
+
+*This section was contributed by Anne Glerum.*
+
+In order to localize deformation under prescribed far-field
+extension, initial weaknesses have to be introduced to the 
+model setup. Here we discuss plugins that 1) perturb the lithosphere
+consisting of upper crust, lower crust and mantle lithosphere
+at a user-specified location and 2) add initial plastic 
+strain is around this same location. This strain represents
+inherited weakness for example from prior deformation phases.
+To represent other deviations of the reference lithosphere,
+additional regions of different lithospheric layer thicknesses
+can also be specified.
+
+The initial temperature plugin prescribes a steady-state
+continental geotherm within the lithosphere and an adiabat
+below. The temperature field is perturbed in the same way
+as the lithosphere compositional structure.
+
+In case the perturbations of the lithosphere in combination with
+the free surface induce large velocities initially, an initial 
+topography plugin approximates the topography resulting from
+isostatic equilibrium. 
+
+
+## Initial lithosphere compositional fields and temperature
+
+```{figure-md} fig:setup
+<img src="Initial_density_with_craton.*" style="width:80.0%" />
+
+Lithospheric structure with perturbations that represent an
+incipient rift and a cratonic region.
+```
+
+The perturbation of the lithospheric layers that represents an
+incipient rift follows a Gaussian
+curve. We can either thicken or thin the layers, depending on 
+the sign of the Gaussian amplitude: a negative amplitude thickens
+the corresponding layer and vice versa. The width of the perturbation
+is determined by the sigma of the Gaussian. The centre of the Gaussian
+curve will be the rift centre. The parameters that need to be set are:
+
+
+```{literalinclude} initial_composition_lithosphere.prm
+```
+
+In addition to a rift centre, other deviations from the reference
+lithospheric thicknesses can also be prescribed. In the above snippet,
+these are specified as polygons (multiple polygons are allowed) with
+their own layer thicknesses. The transition from reference lithosphere
+to polgyon lithosphere is implemented as a hyperbolic tangent with a
+centre point and a half-width.
+
+
+```{literalinclude} initial_temperature.prm
+```
+
+For the initial temperature we combine two plugins: one that prescribes
+a continental steady-state geotherm and one that computes an adiabatic
+temperature profile. The geotherm implementation is based on Chapter 4.6
+of Turcotte and Schubert. For each x-coordinate, it solves a steady-state
+heat conduction equation taking into account the respective densities, 
+heat productivities and thermal conductivities of the three lithospheric
+layers. Below the lithospheric a NaN is returned, such that we can replace
+this NaN by an adiabatic temperature profile. Care has to be taken that the
+adiabatic surface temperature matches the LAB temperature.
+
+```{figure-md} fig:initial_temperature
+<img src="Initial_temperature_with_craton.*" style="width:60.0%" />
+
+ The initial temperature distribution.
+
+```{literalinclude} initial_topography.prm
+```
+
+```{literalinclude} initial_composition_strain.prm
+```
+
+To include inherited heterogeneity we also include initial plastic strain
+in the rift centre (Fig. {numref}`fig:initial_strain`). 
+We generate random strain values between 0 and 1 that
+are subsequently multiplied with a Gaussian distribution for which we specify
+the maximum amplitude and sigma. To control the depth extent of the initial
+strain, we specify a depth around which the amplitude is smoothed to zero
+with a hyperbolic tangent.
+
+```{figure-md} fig:initial_strain
+<img src="Initial_strain_with_craton.*" style="width:60.0%" />
+
+ The initial plastic strain distribution.
+
+```{literalinclude} initial_topography.prm
+```
+
+Sometimes the combination of a free surface with lateral variations in the
+lithospheric thicknesses leads to very high velocities in the first timesteps.
+To avoid a drunken sailor effect and/or very small timesteps, we can then
+prescribe initial topography that roughly fulfills isostatic equilibrium (Fig. {numref}`fig:initial_topography`). 
+The required topography is computed using the reference density, so it neglects
+temperature effects on the density.
+
+
+```{figure-md} fig:initial_topography
+<img src="Initial_topography_with_craton.*" style="width:60.0%" />
+
+ The initial topography that roughly isostatically balances the rift perturbation and craton region
+ with respect to the reference lithosphere.
+```

From 982f9b7c9d244f34cca6853fff8c123981c71988 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 31 May 2024 01:37:47 +0200
Subject: [PATCH 27/38] Add craton and AMR

---
 .../5p_fixed_CERI_craton_right.prm            | 338 ++++++++++++++++++
 .../continental_extension.prm                 | 310 ++++++++++++++++
 ...ns_continental_rift_initial_topography.prm |  17 +-
 ...continental_rift_no_initial_topography.prm |  18 +-
 .../test.prm                                  | 251 +++++++++++++
 5 files changed, 917 insertions(+), 17 deletions(-)
 create mode 100644 cookbooks/initial_conditions_continental_rift/5p_fixed_CERI_craton_right.prm
 create mode 100644 cookbooks/initial_conditions_continental_rift/continental_extension.prm
 create mode 100644 cookbooks/initial_conditions_continental_rift/test.prm

diff --git a/cookbooks/initial_conditions_continental_rift/5p_fixed_CERI_craton_right.prm b/cookbooks/initial_conditions_continental_rift/5p_fixed_CERI_craton_right.prm
new file mode 100644
index 00000000000..103eb58ea4c
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/5p_fixed_CERI_craton_right.prm
@@ -0,0 +1,338 @@
+set Additional shared libraries            = /Applications/ASPECT/VisualStudioCode/aspect/cookbooks/initial_conditions_continental_rift/libinitial_conditions_continental_rift.debug.so
+
+
+set Dimension                              = 2
+set End time                               = 3500
+set Use years in output instead of seconds = true
+set CFL number                             = 1
+set Maximum time step         = 3.5e3
+set Maximum first time step                = 2e2
+set Maximum relative increase in time step = 100
+
+set Adiabatic surface temperature          = 1547
+set Pressure normalization                 = no
+set Output directory = /Applications/ASPECT/VisualStudioCode/aspect/cookbooks/initial_conditions_continental_rift/output
+
+set Nonlinear solver scheme                = single Advection, iterated Stokes
+set Max nonlinear iterations               = 2
+set Nonlinear solver tolerance             = 1e-3
+set Max nonlinear iterations in pre-refinement      = 0
+
+# Solver parameters
+subsection Solver parameters
+  subsection Stokes solver parameters
+    set Number of cheap Stokes solver steps = 1000
+    set Linear solver tolerance             = 1e-3
+    set GMRES solver restart length         = 50
+    set Use full A block as preconditioner  = true
+  end
+end
+
+subsection Geometry model
+  set Model name = box
+
+  subsection Box
+    set X extent = 700e3
+    set Y extent = 300e3
+    set X repetitions = 70
+    set Y repetitions = 30
+  end
+
+end
+
+# Take the minimum of the continental geotherm
+# and the adiabat with 'Adiabatic surface temperature'
+subsection Initial temperature model
+  set List of model names = adiabatic, lithosphere with rift
+  set List of model operators = add, replace if valid
+  subsection Lithosphere with rift
+    set LAB isotherm temperature = 1623.
+    set Surface temperature = 293.
+    # Whether or not to prescribe the LAB depth up to a
+    # certain depth (in area below LAB)
+    # or use adiabat everywhere
+    set Use temperature compensation depth = true
+    set Temperature compensation depth = 200e3
+  end
+  subsection Adiabatic
+    # A reference profile of the compositional fields
+    # where x represents depth
+    subsection Function
+    #  plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio_marine_continental_sediment, silt_fraction
+       set Function expression           = 0; \
+                                           0; \
+                                           0; \
+                                           0; \
+             0; \
+                                           if(x<23e3,1,0); \
+                                           if(x>=23e3&x<43e3,1,0); \
+                                           if(x>=43e3&x<200e3,1,0); \
+                                           0; \
+                                           0
+    end
+    set Age top boundary layer        = 0
+    set Age bottom boundary layer     = 0
+  end
+end
+
+subsection Compositional fields
+  set Number of fields = 10
+  set Names of fields = plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio_marine_continental_sediment, silt_fraction
+end
+
+subsection Initial composition model
+  set List of model names = lithosphere with rift, rift box initial plastic strain, function
+  #set List of model names = lithosphere with rift, rift, function
+  subsection Lithosphere with rift
+    set Blend polygons and rifts                       = true
+    set Standard deviation of Gaussian rift geometry   = 60e3
+    set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
+    # LAB at 110 km
+    set Rift axis line segments                        = 350e3
+    set Layer thicknesses                              = 20e3, 15e3, 85e3
+
+    # Polygon LAB at 200 km
+    set Lithospheric polygon layer thicknesses         = 23e3, 20e3 , 157.e3
+    set Lithospheric polygons                          = 450e3 > 3000e3
+    set Half width of polygon smoothing                = 10e3
+  end
+
+  # Inherited noise
+  subsection Rift box initial plastic strain
+    set Standard deviation of Gaussian noise amplitude distribution   = 200e3
+    set Maximum amplitude of Gaussian noise amplitude distribution      = 0.250000
+    set Random number generator seed                                    = 2
+    set Depth around which Gaussian noise is smoothed out               = 50e3
+    set Halfwidth with which Gaussian noise is smoothed out in depth    = 10e3
+    #set Grid intervals for noise X or radius                            = 2240
+    # Add 16 intervals for the additional 5 km that is added to the grid
+    # to account for initial topography
+    #set Grid intervals for noise Y or longitude                         = 976 #960
+    set Rift axis line segments                                         = 350e3
+  end
+
+  subsection Function
+    set Variable names = x,y
+    set Function expression           = 0; \
+                                        0; \
+                                        0; \
+          0; \
+          0; \
+          0; \
+          0; \
+          0; \
+          0; \
+          0
+  end
+end
+
+subsection Boundary composition model
+  set List of model names = function
+  set Fixed composition boundary indicators = bottom, top
+  subsection Function
+    set Variable names      = x,y,t
+    set Function constants  = h=300e3,My=1e-6, SL=0
+    # Names of fields = plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio, silt_fraction
+    set Function expression = 0; \
+                              0; \
+                              if(y>h/2 && t>0,t*My,0); \
+                              if(y>h/2 && t>0,h+SL-y,0); \
+                              if(y>h/2 && t>0,1,0); \
+                              if(y>h/2 && t==0,1,0); \
+                              0; \
+                              0; \
+                              0; \
+                              0
+  end
+end
+
+subsection Boundary temperature model
+  set List of model names = initial temperature, box
+  set List of model operators = add, minimum
+  set Fixed temperature boundary indicators   = bottom, top
+  subsection Box
+    set Top temperature    =  293
+    set Bottom temperature = 5000   # Unrealistically high, so that it is always taken from initial temperature plugin
+  end
+end
+
+
+subsection Mesh deformation
+  set Additional tangential mesh velocity boundary indicators = right
+  set Mesh deformation boundary indicators = top: free surface, top: ascii data
+
+  subsection Ascii data model
+    set Data directory =  /Applications/ASPECT/VisualStudioCode/aspect/cookbooks/initial_conditions_continental_rift
+    set Data file name = 5p_fixed_craton_UC23km.txt
+  end
+end
+
+subsection Formulation
+  set Formulation          = custom
+  # incompressible
+  set Mass conservation    = ask material model
+  # use reference density in the temperature equation
+  set Temperature equation = reference density profile
+end
+
+subsection Boundary velocity model
+  set Prescribed velocity boundary indicators = left: function, right: function
+  set Tangential velocity boundary indicators =
+  subsection Function
+    set Coordinate system   = cartesian
+    set Variable names      = x,y,t
+    set Function constants  = mm=0.001, yr=1, Z=300e3, X=700e3, outflow=10
+    set Function expression = if(x<X/2,-1,1)*outflow/2*mm/yr; \
+                              0
+  end
+end
+
+subsection Boundary traction model
+  set Prescribed traction boundary indicators = bottom: initial lithostatic pressure
+  subsection Initial lithostatic pressure
+    set Representative point = 10000,0
+  end
+end
+
+
+subsection Gravity model
+  set Model name = vertical
+
+  subsection Vertical
+    set Magnitude = 9.81
+  end
+end
+
+
+subsection Material model
+  set Model name = visco plastic
+  set Material averaging = harmonic average only viscosity
+
+  subsection Visco Plastic
+
+    set Reference temperature = 293
+
+    set Minimum strain rate = 1.e-25
+    set Reference strain rate = 1.e-16
+
+    set Minimum viscosity = 5e18
+    set Maximum viscosity = 1e25
+
+    # bg, plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio_marine_continental_sediment, silt_fraction
+    set Heat capacities       = 1200
+    # Use densities for masked fields that are closest to the density of the area they are in to avoid artefacts from under/overshoot.
+    set Densities             = 3182, 2613, 2758, 2410, 2410, 2410, 2613, 2758, 3163, 2410, 2410
+    set Thermal expansivities = 3.0e-5, 2.7e-5, 2.7e-5, 3.7e-5, 3.7e-5, 3.7e-5, 2.7e-5, 2.7e-5, 3.0e-5, 3.7e-5, 3.7e-5
+    set Define thermal conductivities = true
+    set Thermal conductivities = 3, 2.5, 2.5, 2.1, 2.1, 2.1, 2.5, 2.5, 3, 2.5, 2.5
+
+    set Viscosity averaging scheme = harmonic
+
+    set Viscous flow law = composite
+
+    # Dislocation creep parameters for
+    # 1. Background material/mantle (dry olivine)
+    #    Hirth & Kohlstedt (2003),  Geophys. Monogr. Am. Geophys. Soc., v.138, p.83-105.
+    #    "Rheology of the upper mantle and the mantle wedge:a view from the experimentalists"
+    # 2. Upper crust (wet quartzite)
+    #    Rutter & Brodie (2004), J. Struct. Geol., v.26, p.2011-2023.
+    #    "Experimental grain size-sensitive flow of hot-pressed Brazilian quartz aggregates"
+    # 3. Lower crust and weak seed (wet anorthite)
+    #    Rybacki et al. (2006), J. Geophys. Res., v.111(B3).
+    #    "Influence of water fugacity and activation volume on the flow properties of fine-grained
+    #    anorthite aggregates"
+    # Note that the viscous pre-factors below are scaled to plane strain from unixial strain experiments.
+    set Prefactors for dislocation creep          = 2.12e-15,  1e-20,      1e-20 , 1e-20,      1e-20 , 8.57e-28,  8.57e-28,   7.13e-18,  6.52e-16, 1e-20, 1e-20
+    set Stress exponents for dislocation creep    =      3.5,  1.0  ,       1.0  , 1.0  ,       1.0  , 4.0     ,    4.0   ,      3.0  ,      3.5, 1, 1
+    set Activation energies for dislocation creep =   480.e3, 530.e3,      530.e3, 530.e3,      530.e3, 223.e3  ,   223.e3 ,   345.e3  ,   530.e3, 530.e3, 530e3
+    set Activation volumes for dislocation creep  =   11.e-6, 18.e-6,      18.e-6, 18.e-6,      18.e-6, 0.      ,    0.    ,    38.e-6 ,   18.e-6, 18.e-6, 18e-6
+
+    set Prefactors for diffusion creep          =     1.5e-9, 2.25e-9,      2.25e-9, 2.25e-9,      2.25e-9, 5.97e-19, 5.97e-19,   2.99e-25,  2.25e-9, 2.25e-9, 2.25e-9
+    set Activation energies for diffusion creep =    335.e3 , 375.e3 ,      375.e3 , 375.e3 ,      375.e3 , 223.e3  , 223.e3  ,   159.e3  ,   375.e3, 375e3, 375e3
+    set Activation volumes for diffusion creep  =     4.e-6 , 6.e-6  ,      6.e-6  ,  6.e-6  ,      6.e-6  ,  0.     ,    0.   ,   38.e-6  ,   6.e-6, 6.e-6, 6e-6
+    set Grain size                               =    1e-3
+    set Grain size exponents for diffusion creep =      0.  ,      0.    ,       0.    ,    0.    ,       0.    ,    2    ,   2     ,       3   ,     0, 0, 0
+    # Plasticity parameters
+    set Angles of internal friction = 26.56
+    set Cohesions                   = 5.e6
+
+    # Strain weakening parameters
+    set Strain weakening mechanism  = plastic weakening with plastic strain and viscous weakening with viscous strain
+    set Start plasticity strain weakening intervals = 0.0
+    set End plasticity strain weakening intervals = 2
+    set Cohesion strain weakening factors = 1.0
+    set Friction strain weakening factors = 0.25
+
+    set Start prefactor strain weakening intervals = 0.0
+    set End prefactor strain weakening intervals   = 2
+    # TODO apply weakening to bg as well?
+    set Prefactor strain weakening factors         = 1.0, 1.0, 1.0, 1.0, 1.0, 0.25, 0.25, 0.25, 0.25, 1.0, 1.0
+
+  end
+end
+
+subsection Mesh refinement
+  set Initial global refinement                = 0
+  set Initial adaptive refinement              = 0
+  set Time steps between mesh refinement       = 0
+  set Strategy                                 = minimum refinement function
+  set Skip solvers on initial refinement       = false
+
+  subsection Minimum refinement function
+    set Coordinate system   = cartesian
+    set Variable names      = x,y
+    # Level 5 (highest) in upper 45 km (crust is at most 43 km thick).
+    # Level 3 up to 130 km depth (normal lithosphere is 120 km thick).
+    # Level 3 up to 210 km depth if craton present (craton is 200 km thick).
+    # Level 1 below.
+    set Function expression = if(y>=255e3,5,if(y>90e3, 3, 1))
+  end
+
+end
+
+subsection Heating model
+  set List of model names = compositional heating, adiabatic heating, shear heating
+  subsection Adiabatic heating
+    set Use simplified adiabatic heating = true
+  end
+  subsection Compositional heating
+    # order:                                                  background, plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio, silt_fraction
+    set Use compositional field for heat production averaging =   0     ,      0        ,         0     ,  0      ,  0              , 1           , 1    ,  1   ,     1, 0, 0
+    set Compositional heating values                          =   0     ,      0        ,         0     ,  0      ,  0              , 1.2e-6      ,1.0e-6,0.1e-6,   0, 0, 0
+  end
+end
+
+subsection Adiabatic conditions model
+  set Model name = compute profile
+  subsection Compute profile
+    set Composition reference profile = function
+    # In terms of depth
+    # Moho depth craton 43 km, LAB depth 200 km (i.e. max LAB depth in model)
+    set Function expression           = 0; \
+          0; \
+          0; \
+          0; \
+          0; \
+                                        if(x<23e3,1,0); \
+                                        if(x>=23e3&x<43e3,1,0); \
+                                        if(x>=43e3&x<200e3,1,0); \
+          0; \
+                                        0
+  end
+end
+
+subsection Postprocess
+  set List of postprocessors = velocity statistics, temperature statistics, visualization, composition statistics, topography
+  subsection Visualization
+    set Interpolate output            = false
+    set Write higher order output     = false
+    set List of output variables      = adiabat, viscosity, density, named additional outputs, thermal conductivity, heating
+    set Time between graphical output = 500e3
+    set Point-wise stress and strain  = true
+  end
+  subsection Topography
+    set Output to file = true
+    set Time between text output = 500e3
+  end
+
+end
diff --git a/cookbooks/initial_conditions_continental_rift/continental_extension.prm b/cookbooks/initial_conditions_continental_rift/continental_extension.prm
new file mode 100644
index 00000000000..fba92e9d2da
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/continental_extension.prm
@@ -0,0 +1,310 @@
+#### Continental Extension Cookbook
+# This cookbook is based off numerous published studies, five of which are listed below.
+# For additional information, see these publications and references therein.
+#   1. Brune, S., Heine, C., Perez-Gussinye, M., and Sobolev, S.V. (2014), Nat. Comm., v.5, n.4014,
+#      Rift migration explains continental margin asymmetry and crustal hyperextension
+#   2. Huismans, R., and Beaumont, C. (2011), Nature, v.473, p.71-75.
+#      Depth-dependent extension, two-stage breakup and cratonic underplating at rifted margins
+#   3. Naliboff, J., and Buiter, S.H. (2015), Earth Planet. Sci. Lett., v.421, p.58-67,
+#      "Rift Reactivation and migration during multiphase extension"
+#   4. Naliboff, J., Glerum, A., Sascha, S., Peron-Pinvidic, G., and Wrona, T. (2020), Geophys.
+#      Res. Lett., 47, e2019GL086611, "Development of 3‐D rift heterogeneity through fault
+#      network evolution"
+#   5. Sandiford, D., Brune, S., Glerum, A., Naliboff, J., and Whittaker, J.M. (2021), Geophys.
+#      Geochem. Geosys., 22, e2021GC009681, "Kinematics of footwall exhumation at oceanic
+#      detachment faults: Solid-block rotation and apparent unbending"
+
+####  Global parameters
+set Additional shared libraries            = /Applications/ASPECT/VisualStudioCode/aspect/cookbooks/initial_conditions_continental_rift/libinitial_conditions_continental_rift.debug.so
+set Dimension                              = 2
+set Start time                             = 0
+set End time                               = 2e3
+set Use years in output instead of seconds = true
+set Nonlinear solver scheme                = single Advection, iterated Stokes
+set Nonlinear solver tolerance             = 1e-4
+set Max nonlinear iterations               = 1
+set CFL number                             = 0.5
+set Maximum time step                      = 2e3
+set Output directory                       = output-continental_extension
+set Pressure normalization                 = no
+
+#### Parameters describing the model
+
+# Governing equations
+subsection Formulation
+  set Formulation = Boussinesq approximation
+end
+
+# Model geometry (200x100 km, 20 km spacing)
+subsection Geometry model
+  set Model name = box
+
+  subsection Box
+    set X repetitions = 70
+    set Y repetitions = 30
+    set X extent      = 700e3
+    set Y extent      = 300e3
+  end
+end
+
+subsection Mesh refinement
+  set Initial adaptive refinement        = 0
+  set Initial global refinement          = 0
+  set Time steps between mesh refinement = 0
+  set Strategy = minimum refinement function
+
+  subsection Minimum refinement function
+    set Coordinate system   = cartesian
+    set Variable names      = x,y
+    set Function expression = if ( y>=50e3 && x>=40.e3 && x<=160.e3, 4, 3)
+  end
+end
+
+subsection Solver parameters
+  subsection Stokes solver parameters
+    set Number of cheap Stokes solver steps = 0
+    set Linear solver tolerance = 1e-5
+  end
+
+end
+
+# Advecting the free surface using a normal, rather than vertical,
+# projection. To reduce mesh instabilities and associated solver
+# issues when deformation becomes large, diffusion is applied to
+# the free surface at each time step.
+subsection Mesh deformation
+  set Mesh deformation boundary indicators        = top: free surface
+
+  subsection Free surface
+    set Surface velocity projection = normal
+  end
+
+end
+
+# Velocity on boundaries characterized by functions
+# The outward velocity (x-direction) on the left and right walls is 0.25 cm/year
+# The vertical velocity at the base is 0.25 cm/year (balances outflow on sides)
+# Velocity components parallel to the base (x-velocity) and side walls (y-velocity)
+# are unconstrained (i.e. 'free').
+subsection Boundary velocity model
+  set Prescribed velocity boundary indicators = left x: function, right x:function
+
+  subsection Function
+    set Variable names      = x,y
+    set Function constants  = v=0.0025, w=700.e3, d=300.e3
+    set Function expression = if (x < w/2 , -v, v) ; v*2*d/w
+  end
+end
+
+subsection Boundary traction model
+  set Prescribed traction boundary indicators = bottom: initial lithostatic pressure
+  subsection Initial lithostatic pressure
+    set Representative point = 10000,0
+  end
+end
+# Number and names of compositional fields
+# The five compositional fields represent:
+# 1. The plastic strain that accumualates over time, with the initial plastic strain removed
+# 2. The plastic strain that accumulated over time, including the initial plastic strain values
+# 3. The upper crust
+# 4. The lower crust
+# 5. The mantle lithosphere
+subsection Compositional fields
+  set Number of fields = 5
+  set Names of fields = noninitial_plastic_strain, plastic_strain, upper, lower, mantle_L
+end
+
+# Initial values of different compositional fields
+# The upper crust (20 km thick), lower crust (20 km thick)
+# and mantle (60 km thick) are continuous horizontal layers
+# of constant thickness. The non initial plastic strain is set
+# to 0 and the initial plastic strain is randomized between
+# 0.5 and 1.5.
+subsection Initial composition model
+  set List of model names = rift box initial plastic strain, function
+
+  subsection Rift box initial plastic strain
+    set Standard deviation of Gaussian noise amplitude distribution   = 200e3
+    set Maximum amplitude of Gaussian noise amplitude distribution      = 0.250000
+    set Random number generator seed                                    = 2.000000
+    set Depth around which Gaussian noise is smoothed out               = 50e3
+    set Halfwidth with which Gaussian noise is smoothed out in depth    = 10e3
+    set Rift axis line segments                                         = 350e3
+  end
+  subsection Function
+    set Variable names      = x,y
+    set Function expression = 0; \
+                              0; \
+                              if(y>=280.e3, 1, 0); \
+                              if(y<280.e3 && y>=260.e3, 1, 0); \
+                              if(y<260.e3, 1, 0);
+  end
+end
+
+# Composition: fixed on bottom (inflow boundary), free on sides and top
+subsection Boundary composition model
+  set Fixed composition boundary indicators = bottom
+  set List of model names = initial composition
+end
+
+# Temperature boundary conditions
+# Top and bottom (fixed) temperatures are consistent with the initial temperature field
+# Note that while temperatures are specified for the model sides, these values are
+# not used as the sides are not specified "Fixed temperature boundaries".  Rather,
+# these boundaries are insulating (zero net heat flux).
+subsection Boundary temperature model
+  set Fixed temperature boundary indicators = bottom, top
+  set List of model names = box
+
+  subsection Box
+    set Bottom temperature = 1613
+    set Top temperature    =  273
+  end
+end
+
+# Initial temperature field
+# Typical continental geotherm based on equations 4-6 from:
+#   D.S. Chapman (1986), "Thermal gradients in the continental crust",
+#   Geological Society of London Special Publications, v.24, p.63-70.
+# The initial constraints are:
+#   Surface Temperature  - upper crust (ts1) = 273 K
+#   Surface Heat Flow    - upper crust (qs1) = 0.055 mW/m^2
+#   Heat Production      - upper crust (A1)  = 1.00e-6 W/m^3;
+#   Heat Production      - lower crust (A2)  = 0.25e-6 W/m^3;
+#   Heat Production      - mantle (A3)       = 0.00e-6 W/m^3;
+#   Thermal Conductivity - all layers        = 2.5 (W/(m K));
+# To satisfy these constraints, the following values are required:
+#   Surface Temperature  - lower crust (ts2) = 633 K
+#                        - mantle (ts3)      = 893 K
+#   Surface Heat Flow    - lower crust (qs2) = 0.035 W/m^2;
+#                        - mantle      (qs3) = 0.030 W/m^2;
+# Note: The continental geotherm initial temperature model
+#       plugin can be used to compute an identical geotherm
+#       for the lithosphere. An example of how to use this
+#       plugin is illustrated in the test for this cookbook
+#       (tests/continental_extension.prm).
+subsection Initial temperature model
+  set Model name = function
+
+  subsection Function
+    set Variable names = x,y
+    set Function constants = h=100e3, ts1=273, ts2=633, ts3=893, \
+                             A1=1.e-6, A2=0.25e-6, A3=0.0, \
+                             k1=2.5, k2=2.5, k3=2.5, \
+                             qs1=0.055, qs2=0.035, qs3=0.030
+    set Function expression = if( (h-y)<=20.e3, \
+                                  ts1 + (qs1/k1)*(h-y) - (A1*(h-y)*(h-y))/(2.0*k1), \
+                                  if( (h-y)>20.e3 && (h-y)<=40.e3, \
+                                      ts2 + (qs2/k2)*(h-y-20.e3) - (A2*(h-y-20.e3)*(h-y-20.e3))/(2.0*k2), \
+                                      ts3 + (qs3/k3)*(h-y-40.e3) - (A3*(h-y-40.e3)*(h-y-40.e3))/(2.0*k3) ) );
+  end
+end
+
+# Constant internal heat production values (W/m^3) for background material
+# and compositional fields.
+subsection Heating model
+  set List of model names = compositional heating
+
+  subsection Compositional heating
+    set Use compositional field for heat production averaging = 1, 0, 0, 1, 1, 1
+    set Compositional heating values = 0.0, 0.0, 0.0, 1.0e-6, 0.25e-6, 0.
+  end
+end
+
+# Material model
+# Rheology: Non-linear viscous flow and Drucker Prager Plasticity
+# Values for most rheological parameters are specified for a background material and
+# each compositional field.  Values for viscous deformation are based on dislocation
+# creep flow-laws, with distinct values for the upper crust (wet quartzite), lower
+# crust (wet anorthite) and mantle (dry olivine).  Table 1 of Naliboff and Buiter (2015),
+# Earth Planet. Sci. Lett., v.421, p. 58-67 contains values for each of these flow laws.
+subsection Material model
+  set Model name = visco plastic
+
+  subsection Visco Plastic
+    # Reference temperature and viscosity
+    set Reference temperature = 273
+
+    # The minimum strain-rate helps limit large viscosities values that arise
+    # as the strain-rate approaches zero.
+    # The reference strain-rate is used on the first non-linear iteration
+    # of the first time step when the velocity has not been determined yet.
+    set Minimum strain rate = 1.e-20
+    set Reference strain rate = 1.e-16
+
+    # Limit the viscosity with minimum and maximum values
+    set Minimum viscosity = 1e18
+    set Maximum viscosity = 1e26
+
+    # Thermal diffusivity is adjusted to match thermal conductivities
+    # assumed in assigning the initial geotherm
+    set Define thermal conductivities = true
+    set Thermal conductivities        = 2.5
+    set Heat capacities               = 750.
+
+    # Density values of 1 are assigned to "strain" fields, which are not taken into
+    # account when computing material properties.
+    set Densities                     = 3300, 1.0, 1.0, 2700,  2900, 3300
+    set Thermal expansivities         = 2e-5
+
+    # Harmonic viscosity averaging
+    set Viscosity averaging scheme = harmonic
+
+    # Choose to have the viscosity (pre-yield) follow a dislocation
+    # diffusion or composite flow law.  Here, dislocation is selected
+    # so no need to specify diffusion creep parameters below, which are
+    # only used if "diffusion" or "composite" option is selected.
+    set Viscous flow law = dislocation
+
+    # Dislocation creep parameters for
+    # 1. Background material/mantle (dry olivine)
+    #    Hirth & Kohlstedt (2004),  Geophys. Monogr. Am. Geophys. Soc., v.138, p.83-105.
+    #    "Rheology of the upper mantle and the mantle wedge:a view from the experimentalists"
+    # 2. Upper crust (wet quartzite)
+    #    Rutter & Brodie (2004), J. Struct. Geol., v.26, p.2011-2023.
+    #    "Experimental grain size-sensitive flow of hot-pressed Brazilian quartz aggregates"
+    # 3. Lower crust and weak seed (wet anorthite)
+    #    Rybacki et al. (2006), J. Geophys. Res., v.111(B3).
+    #    "Influence of water fugacity and activation volume on the flow properties of fine-grained
+    #    anorthite aggregates"
+    # Note that the viscous pre-factors below are scaled to plane strain from unixial strain experiments.
+    # For ease of identification, fields tracking strain are assigned prefactors of 1e-50
+    set Prefactors for dislocation creep          = 6.52e-16, 1.00e-50, 1.00e-50, 8.57e-28, 7.13e-18, 6.52e-16
+    set Stress exponents for dislocation creep    =      3.5,      1.0,      1.0,      4.0,      3.0,      3.5
+    set Activation energies for dislocation creep =   530.e3,      0.0,      0.0,   223.e3,   345.e3,   530.e3
+    set Activation volumes for dislocation creep  =   18.e-6,      0.0,      0.0,      0.0,      0.0,   18.e-6
+
+    # Plasticity parameters
+    set Angles of internal friction = 30
+    set Cohesions                   = 20.e6
+
+    # The parameters below weaken the friction and cohesion by a
+    # a factor of 4 between plastic strain values of 0.5 and 1.5.
+    set Strain weakening mechanism                   = plastic weakening with plastic strain only
+    set Start plasticity strain weakening intervals  = 0.5
+    set End plasticity strain weakening intervals    = 1.5
+    set Cohesion strain weakening factors            = 0.25
+    set Friction strain weakening factors            = 0.25
+  end
+end
+
+# Gravity model
+subsection Gravity model
+  set Model name = vertical
+
+  subsection Vertical
+    set Magnitude = 9.81
+  end
+end
+
+# Post processing
+subsection Postprocess
+  set List of postprocessors = composition statistics, heat flux densities, heat flux statistics, mass flux statistics, pressure statistics, temperature statistics, topography, velocity statistics, visualization
+
+  subsection Visualization
+    set List of output variables = density, named additional outputs, strain rate, viscosity
+    set Output format                 = vtu
+    set Time between graphical output = 100.e3
+    set Interpolate output            = true
+  end
+end
diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
index 5621f14a757..e662e023563 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
@@ -13,7 +13,7 @@ set Nonlinear solver tolerance             = 1e-5
 set Max nonlinear iterations               = 2
 set CFL number                             = 0.5
 set Maximum time step                      = 20e3
-set Output directory                       = output-initial_conditions_continental_rift_initial_topography
+set Output directory                       = output-initial_conditions_continental_rift_initial_topography_with_craton
 set Pressure normalization                 = no
 set Adiabatic surface temperature          = 1573
 
@@ -44,13 +44,14 @@ subsection Geometry model
 
 end
 
-# Globally refine the mesh to 2.5 km spacing, and then
-# adaptively refine the mesh to 1.25 km spacing above y=50 km
-# and between x=40 and x=160 km. These values ensure areas
+
+# Globally refine the mesh to 5 km spacing, and then
+# adaptively refine the mesh to 2.5 km spacing for the crustal layers.
+# These values ensure areas
 # undergoing brittle deformation are in the high-resolution
 # region.
 subsection Mesh refinement
-  set Initial adaptive refinement        = 0
+  set Initial adaptive refinement        = 1
   set Initial global refinement          = 3
   set Time steps between mesh refinement = 0
   set Strategy = minimum refinement function
@@ -58,7 +59,7 @@ subsection Mesh refinement
   subsection Minimum refinement function
     set Coordinate system   = cartesian
     set Variable names      = x,y
-    set Function expression = if ( y>=50e3 && x>=40.e3 && x<=160.e3, 4, 3)
+    set Function expression = if ( y>= 155e3, 4, 3)
   end
 end
 
@@ -148,7 +149,7 @@ subsection Initial composition model
     # The thicknesses of the lithospheric layer within a polygon
     set Lithospheric polygon layer thicknesses         = 20e3, 15e3 , 115.e3
     # The segments making up the polygon
-    set Lithospheric polygons                          = 550e3 > 3000e3
+    set Lithospheric polygons                          = 350e3 > 3000e3
     # The half width of the transition from polygon to reference lithosphere
     set Half width of polygon smoothing                = 10e3
   end
@@ -284,7 +285,7 @@ subsection Material model
 
     # Density values of 1 are assigned to "strain" fields, which are not taken into
     # account when computing material properties.
-    set Densities                     = 3300, 1.0, 1.0, 2700,  2900, 3300
+    set Densities                     = 3300, 1.0, 1.0, 2700,  2900, 3200
     set Thermal expansivities         = 2e-5
 
     # Harmonic viscosity averaging
diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
index 56fc5a19662..2472ad4884d 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
@@ -6,14 +6,14 @@
 set Additional shared libraries            = $ASPECT_SOURCE_DIR/cookbooks/initial_conditions_continental_rift/libinitial_conditions_continental_rift.debug.so
 set Dimension                              = 2
 set Start time                             = 0
-set End time                               = 0 #5e6
+set End time                               = 0
 set Use years in output instead of seconds = true
 set Nonlinear solver scheme                = single Advection, iterated Stokes
 set Nonlinear solver tolerance             = 1e-5
-set Max nonlinear iterations               = 2
+set Max nonlinear iterations               = 50
 set CFL number                             = 0.5
 set Maximum time step                      = 20e3
-set Output directory                       = output-initial_conditions_continental_rift_no_initial_topography
+set Output directory                       = output-initial_conditions_continental_rift_no_initial_topography_with_craton
 set Pressure normalization                 = no
 set Adiabatic surface temperature          = 1573
 
@@ -36,13 +36,13 @@ subsection Geometry model
   end
 end
 
-# Globally refine the mesh to 2.5 km spacing, and then
-# adaptively refine the mesh to 1.25 km spacing above y=50 km
-# and between x=40 and x=160 km. These values ensure areas
+# Globally refine the mesh to 5 km spacing, and then
+# adaptively refine the mesh to 2.5 km spacing for the crustal layers.
+# These values ensure areas
 # undergoing brittle deformation are in the high-resolution
 # region.
 subsection Mesh refinement
-  set Initial adaptive refinement        = 0
+  set Initial adaptive refinement        = 1
   set Initial global refinement          = 3
   set Time steps between mesh refinement = 0
   set Strategy = minimum refinement function
@@ -50,7 +50,7 @@ subsection Mesh refinement
   subsection Minimum refinement function
     set Coordinate system   = cartesian
     set Variable names      = x,y
-    set Function expression = if ( y>=50e3 && x>=40.e3 && x<=160.e3, 4, 3)
+    set Function expression = if ( y>= 155e3, 4, 3)
   end
 end
 
@@ -140,7 +140,7 @@ subsection Initial composition model
     # The thicknesses of the lithospheric layer within a polygon
     set Lithospheric polygon layer thicknesses         = 20e3, 15e3 , 115.e3
     # The segments making up the polygon
-    set Lithospheric polygons                          = 550e3 > 3000e3
+    set Lithospheric polygons                          = 350e3 > 3000e3
     # The half width of the transition from polygon to reference lithosphere
     set Half width of polygon smoothing                = 10e3
   end
diff --git a/cookbooks/initial_conditions_continental_rift/test.prm b/cookbooks/initial_conditions_continental_rift/test.prm
new file mode 100644
index 00000000000..ac93ccba0cd
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/test.prm
@@ -0,0 +1,251 @@
+#set Additional shared libraries            = /Applications/ASPECT/VisualStudioCode/aspect/cookbooks/initial_conditions_continental_rift/libinitial_conditions_continental_rift.debug.so
+
+set Dimension                              = 2
+set End time                               = 3.5e3
+set Use years in output instead of seconds = true
+set Maximum time step         = 3.5e3
+set Maximum first time step                = 2e2
+set Maximum relative increase in time step = 100
+
+set Adiabatic surface temperature          = 1547
+set Pressure normalization                 = no
+set Output directory = /Applications/ASPECT/VisualStudioCode/aspect/cookbooks/initial_conditions_continental_rift/output
+
+set Nonlinear solver scheme                = single Advection, iterated Stokes
+set Max nonlinear iterations               = 2
+set Nonlinear solver tolerance             = 1e-6
+set Max nonlinear iterations in pre-refinement      = 0
+
+
+subsection Geometry model
+  set Model name = box
+
+  subsection Box
+    set X extent = 700e3
+    set Y extent = 300e3
+    set X repetitions = 70
+    set Y repetitions = 30
+  end
+  subsection Initial topography model
+    set Model name = lithosphere with rift
+  end
+end
+
+subsection Initial temperature model
+  set List of model names = adiabatic
+  subsection Adiabatic
+    subsection Function
+    #  plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio_marine_continental_sediment, silt_fraction
+       set Function expression           = 0; \
+                                           0; \
+                                           0; \
+                                           0; \
+             0; \
+                                           if(x<23e3,1,0); \
+                                           if(x>=23e3&x<43e3,1,0); \
+                                           if(x>=43e3&x<200e3,1,0); \
+                                           0; \
+                                           0
+    end
+    set Age top boundary layer        = 0
+    set Age bottom boundary layer     = 0
+  end
+end
+
+subsection Compositional fields
+  set Number of fields = 10
+  set Names of fields = plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio_marine_continental_sediment, silt_fraction
+end
+
+subsection Initial composition model
+  set List of model names = function
+
+  subsection Function
+    set Variable names = x,y
+    set Function expression           = 0; \
+                                        0; \
+                                        0; \
+          0; \
+          0; \
+          0; \
+          0; \
+          0; \
+          0; \
+          0
+  end
+end
+
+subsection Boundary composition model
+  set List of model names = function
+  set Fixed composition boundary indicators = bottom, top
+  subsection Function
+    set Function expression = 0; \
+                              0; \
+                              0; \
+                              0; \
+                              0; \
+                              0; \
+                              0; \
+                              0; \
+                              0; \
+                              0
+  end
+end
+
+subsection Boundary temperature model
+  set List of model names = box
+  set Fixed temperature boundary indicators   = bottom, top
+  subsection Box
+    set Top temperature    =  293
+    set Bottom temperature = 1700   # Unrealistically high, so that it is always taken from initial temperature plugin
+  end
+end
+
+
+subsection Mesh deformation
+  set Mesh deformation boundary indicators = top: free surface
+end
+
+subsection Formulation
+  set Formulation          = custom
+  # incompressible
+  set Mass conservation    = ask material model
+  # use reference density in the temperature equation
+  set Temperature equation = reference density profile
+end
+
+subsection Boundary velocity model
+  set Tangential velocity boundary indicators = left, right, bottom
+end
+
+
+subsection Gravity model
+  set Model name = vertical
+
+  subsection Vertical
+    set Magnitude = 9.81
+  end
+end
+
+
+subsection Material model
+  set Model name = visco plastic
+  set Material averaging = harmonic average only viscosity
+
+  subsection Visco Plastic
+
+    set Reference temperature = 293
+
+    set Minimum strain rate = 1.e-25
+    set Reference strain rate = 1.e-16
+
+    set Minimum viscosity = 5e18
+    set Maximum viscosity = 1e25
+
+    # bg, plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio_marine_continental_sediment, silt_fraction
+    set Heat capacities       = 1200
+    # Use densities for masked fields that are closest to the density of the area they are in to avoid artefacts from under/overshoot.
+    set Densities             = 3182, 2613, 2758, 2410, 2410, 2410, 2613, 2758, 3163, 2410, 2410
+    set Thermal expansivities = 3.0e-5, 2.7e-5, 2.7e-5, 3.7e-5, 3.7e-5, 3.7e-5, 2.7e-5, 2.7e-5, 3.0e-5, 3.7e-5, 3.7e-5
+    set Define thermal conductivities = true
+    set Thermal conductivities = 3, 2.5, 2.5, 2.1, 2.1, 2.1, 2.5, 2.5, 3, 2.5, 2.5
+
+    set Viscosity averaging scheme = harmonic
+
+    set Viscous flow law = composite
+
+    # Dislocation creep parameters for
+    # 1. Background material/mantle (dry olivine)
+    #    Hirth & Kohlstedt (2003),  Geophys. Monogr. Am. Geophys. Soc., v.138, p.83-105.
+    #    "Rheology of the upper mantle and the mantle wedge:a view from the experimentalists"
+    # 2. Upper crust (wet quartzite)
+    #    Rutter & Brodie (2004), J. Struct. Geol., v.26, p.2011-2023.
+    #    "Experimental grain size-sensitive flow of hot-pressed Brazilian quartz aggregates"
+    # 3. Lower crust and weak seed (wet anorthite)
+    #    Rybacki et al. (2006), J. Geophys. Res., v.111(B3).
+    #    "Influence of water fugacity and activation volume on the flow properties of fine-grained
+    #    anorthite aggregates"
+    # Note that the viscous pre-factors below are scaled to plane strain from unixial strain experiments.
+    set Prefactors for dislocation creep          = 2.12e-15,  1e-20,      1e-20 , 1e-20,      1e-20 , 8.57e-28,  8.57e-28,   7.13e-18,  6.52e-16, 1e-20, 1e-20
+    set Stress exponents for dislocation creep    =      3.5,  1.0  ,       1.0  , 1.0  ,       1.0  , 4.0     ,    4.0   ,      3.0  ,      3.5, 1, 1
+    set Activation energies for dislocation creep =   480.e3, 530.e3,      530.e3, 530.e3,      530.e3, 223.e3  ,   223.e3 ,   345.e3  ,   530.e3, 530.e3, 530e3
+    set Activation volumes for dislocation creep  =   11.e-6, 18.e-6,      18.e-6, 18.e-6,      18.e-6, 0.      ,    0.    ,    38.e-6 ,   18.e-6, 18.e-6, 18e-6
+
+    set Prefactors for diffusion creep          =     1.5e-9, 2.25e-9,      2.25e-9, 2.25e-9,      2.25e-9, 5.97e-19, 5.97e-19,   2.99e-25,  2.25e-9, 2.25e-9, 2.25e-9
+    set Activation energies for diffusion creep =    335.e3 , 375.e3 ,      375.e3 , 375.e3 ,      375.e3 , 223.e3  , 223.e3  ,   159.e3  ,   375.e3, 375e3, 375e3
+    set Activation volumes for diffusion creep  =     4.e-6 , 6.e-6  ,      6.e-6  ,  6.e-6  ,      6.e-6  ,  0.     ,    0.   ,   38.e-6  ,   6.e-6, 6.e-6, 6e-6
+    set Grain size                               =    1e-3
+    set Grain size exponents for diffusion creep =      0.  ,      0.    ,       0.    ,    0.    ,       0.    ,    2    ,   2     ,       3   ,     0, 0, 0
+    # Plasticity parameters
+    set Angles of internal friction = 26.56
+    set Cohesions                   = 5.e6
+
+    # Strain weakening parameters
+    set Strain weakening mechanism  = plastic weakening with plastic strain and viscous weakening with viscous strain
+    set Start plasticity strain weakening intervals = 0.0
+    set End plasticity strain weakening intervals = 2
+    set Cohesion strain weakening factors = 1.0
+    set Friction strain weakening factors = 0.25
+
+    set Start prefactor strain weakening intervals = 0.0
+    set End prefactor strain weakening intervals   = 2
+    # TODO apply weakening to bg as well?
+    set Prefactor strain weakening factors         = 1.0, 1.0, 1.0, 1.0, 1.0, 0.25, 0.25, 0.25, 0.25, 1.0, 1.0
+
+  end
+end
+
+subsection Mesh refinement
+  set Initial global refinement                = 2
+  set Initial adaptive refinement              = 0 #3
+  set Time steps between mesh refinement       = 0
+  set Strategy                                 = minimum refinement function
+  set Skip solvers on initial refinement       = false
+
+  subsection Minimum refinement function
+    set Coordinate system   = cartesian
+    set Variable names      = x,y
+    # Level 5 (highest) in upper 45 km (crust is at most 43 km thick).
+    # Level 3 up to 130 km depth (normal lithosphere is 120 km thick).
+    # Level 3 up to 210 km depth if craton present (craton is 200 km thick).
+    # Level 1 below.
+    set Function expression = if(y>=255e3,5,if(y>90e3, 3, 1))
+  end
+
+end
+
+subsection Heating model
+  set List of model names = compositional heating, adiabatic heating, shear heating
+  subsection Adiabatic heating
+    set Use simplified adiabatic heating = true
+  end
+  subsection Compositional heating
+    # order:                                                  background, plastic_strain, viscous_strain, sediment_age, deposition_depth, sediment, upper, lower, mantle_L, ratio, silt_fraction
+    set Use compositional field for heat production averaging =   0     ,      0        ,         0     ,  0      ,  0              , 1           , 1    ,  1   ,     1, 0, 0
+    set Compositional heating values                          =   0     ,      0        ,         0     ,  0      ,  0              , 1.2e-6      ,1.0e-6,0.1e-6,   0, 0, 0
+  end
+end
+
+subsection Adiabatic conditions model
+  set Model name = compute profile
+  subsection Compute profile
+    set Composition reference profile = function
+    # In terms of depth
+    # Moho depth craton 43 km, LAB depth 200 km (i.e. max LAB depth in model)
+    set Function expression           = 0; \
+          0; \
+          0; \
+          0; \
+          0; \
+                                        if(x<23e3,1,0); \
+                                        if(x>=23e3&x<43e3,1,0); \
+                                        if(x>=43e3&x<200e3,1,0); \
+          0; \
+                                        0
+  end
+end
+
+subsection Postprocess
+  set List of postprocessors = velocity statistics
+
+end

From aaf632569790299e2cf232d23263cd97202512bb Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 31 May 2024 01:38:49 +0200
Subject: [PATCH 28/38] Update topo plugins

---
 .../lithosphere_rift_topo.cc                  | 69 ++++++++-----------
 .../lithosphere_rift_topo.h                   | 18 -----
 2 files changed, 29 insertions(+), 58 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
index 2d27751e897..dee6b5d1003 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -57,13 +57,11 @@ namespace aspect
         }
 
       // Get the relevant densities for the lithosphere.
+      // We take the reference density of the first phase.
       densities.push_back(densities_per_composition[0][0]);
       densities.push_back(densities_per_composition[id_upper+1][0]);
       densities.push_back(densities_per_composition[id_lower+1][0]);
       densities.push_back(densities_per_composition[id_mantle_L+1][0]);
-      std::cout << "Assembling final densities: " << densities_per_composition[0][0] << ", ";
-      std::cout << densities_per_composition[id_upper+1][0] << ", " << densities_per_composition[id_lower+1][0];
-      std::cout  << ", " <<  densities_per_composition[id_mantle_L+1][0] <<  std::endl;
 
       // The reference column
       ref_rgh = 0;
@@ -74,9 +72,6 @@ namespace aspect
       // The total lithosphere thickness
       const double sum_thicknesses = std::accumulate(reference_thicknesses.begin(), reference_thicknesses.end(), 0);
 
-      // Make sure the compensation depth is in the sublithospheric mantle
-      compensation_depth = 2. * sum_thicknesses + 1e3;
-
       // The column at the rift center
       double rift_rgh = 0;
       rift_thicknesses = reference_thicknesses;
@@ -93,6 +88,7 @@ namespace aspect
       const unsigned int n_polygons = polygon_thicknesses.size();
       std::vector<double> polygon_rgh(n_polygons);
       std::vector<double> sum_polygon_thicknesses(n_polygons);
+      double max_sum_polygon_thicknesses = 0.;
       for (unsigned int i_polygons=0; i_polygons<n_polygons; ++i_polygons)
         {
           for (unsigned int l=0; l<3; ++l)
@@ -101,25 +97,32 @@ namespace aspect
             }
           // The total lithosphere thickness
           sum_polygon_thicknesses[i_polygons] = std::accumulate(polygon_thicknesses[i_polygons].begin(), polygon_thicknesses[i_polygons].end(),0);
-          polygon_rgh[i_polygons] += (compensation_depth - sum_polygon_thicknesses[i_polygons]) * densities[0];
+          max_sum_polygon_thicknesses = std::max(max_sum_polygon_thicknesses, sum_polygon_thicknesses[i_polygons]);
+
         }
 
-      // Add sublithospheric mantle part to the columns
-      ref_rgh += (compensation_depth - sum_thicknesses) * densities[0];
-      rift_rgh += (compensation_depth - sum_rift_thicknesses) * densities[0];
+        // Make sure the compensation depth is in the sublithospheric mantle
+        compensation_depth = std::max(sum_thicknesses, std::max(sum_rift_thicknesses, max_sum_polygon_thicknesses)) + 5e3;
 
-      // Compute the maximum topography based on mass surplus/deficit
-      topo_rift_amplitude = (ref_rgh-rift_rgh) / densities[0];
-      for (unsigned int i_polygons=0; i_polygons<n_polygons; ++i_polygons)
-        topo_polygon_amplitude = std::max((ref_rgh-polygon_rgh[i_polygons]) / densities[0],topo_polygon_amplitude);
+        // Add sublithospheric mantle part to the columns
+        ref_rgh += (compensation_depth - sum_thicknesses) * densities[0];
+        rift_rgh += (compensation_depth - sum_rift_thicknesses) * densities[0];
+        for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
+        {
+          polygon_rgh[i_polygons] += (compensation_depth - sum_polygon_thicknesses[i_polygons]) * densities[0];
+        }
 
-      // TODO: probably there are combinations of rift and polygon topography
-      // that result in a higher topography
-      maximum_topography = std::max(topo_rift_amplitude, topo_polygon_amplitude);
+        // Compute the maximum topography based on mass surplus/deficit
+        topo_rift_amplitude = (ref_rgh - rift_rgh) / densities[0];
+        for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
+          topo_polygon_amplitude = std::max((ref_rgh - polygon_rgh[i_polygons]) / densities[0], topo_polygon_amplitude);
 
-      this->get_pcout() << "   Maximum initial topography of rift: " << topo_rift_amplitude << " m" << std::endl;
-      this->get_pcout() << "   Maximum initial topography of polygon: " << topo_polygon_amplitude << " m" << std::endl;
+        // TODO: probably there are combinations of rift and polygon topography
+        // that result in a higher topography
+        maximum_topography = std::max(topo_rift_amplitude, topo_polygon_amplitude);
 
+        this->get_pcout() << "   Maximum initial topography of rift: " << topo_rift_amplitude << " m" << std::endl;
+        this->get_pcout() << "   Maximum initial topography of polygon: " << topo_polygon_amplitude << " m" << std::endl;
     }
 
 
@@ -134,37 +137,26 @@ namespace aspect
       // here.
       if (initial_composition_manager == nullptr)
         const_cast<std::shared_ptr<const aspect::InitialComposition::Manager<dim>>&>(initial_composition_manager) = this->get_initial_composition_manager_pointer();
+
       // Check that the required initial composition model is used
       // We have to do it here instead of in initialize() because
       // the names are not available upon initialization of the
       // initial topography model yet.
       const std::vector<std::string> active_initial_composition_models = initial_composition_manager->get_active_initial_composition_names();
-      AssertThrow(std::find(active_initial_composition_models.begin(),active_initial_composition_models.end(), "lithosphere with rift") != active_initial_composition_models.end(),
-                  ExcMessage("The lithosphere with rift initial mesh refinement plugin requires the lithosphere with rift initial composition plugin."));
+      AssertThrow(initial_composition_manager->template has_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>(),
+                  ExcMessage("The 'lithosphere with rift' initial topography plugin requires the 'lithosphere with rift' initial composition plugin."));
 
-      // When cartesian, position contains x(,y); when spherical, position contains lon(,lat) (in degrees);
+      // When cartesian, position contains x(,y); when spherical, position contains lon(,lat) (in degrees).
       // Turn into a Point<dim-1>
       Point<dim-1> surface_position;
       for (unsigned int d=0; d<dim-1; ++d)
         surface_position[d] = position[d];
 
-      // Get the distance to the line segments along a path parallel to the surface
-      double distance_to_rift_axis = 1e23;
-      std::pair<double,unsigned int> distance_to_L_polygon;
-      for (typename std::list<std::unique_ptr<InitialComposition::Interface<dim>>>::const_iterator it = initial_composition_manager->get_active_initial_composition_conditions().begin();
-           it != initial_composition_manager->get_active_initial_composition_conditions().end();
-           ++it)
-        if ( InitialComposition::LithosphereRift<dim> *ic = dynamic_cast<InitialComposition::LithosphereRift<dim> *> ((*it).get()))
-          {
-            distance_to_rift_axis = ic->distance_to_rift(surface_position);
-            distance_to_L_polygon = ic->distance_to_polygon(surface_position);
-          }
+      // Get the initial composition plugin
+      const InitialComposition::LithosphereRift<dim> &ic = initial_composition_manager->template get_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>();
 
       // Compute the topography based on distance to the rift and distance to the polygon
-      std::vector<double> local_thicknesses(3);
-      local_thicknesses[0] = ((0.5 + 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * polygon_thicknesses[distance_to_L_polygon.second][0] + (0.5 - 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * reference_thicknesses[0]) * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0. - 2. * sigma_polygon ? 1. : (1.0 - A_rift[0] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))));
-      local_thicknesses[1] = ((0.5 + 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * polygon_thicknesses[distance_to_L_polygon.second][1] + (0.5 - 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * reference_thicknesses[1]) * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0. - 2. * sigma_polygon ? 1. : (1.0 - A_rift[1] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))));
-      local_thicknesses[2] = ((0.5 + 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * polygon_thicknesses[distance_to_L_polygon.second][2] + (0.5 - 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon)) * reference_thicknesses[2]) * (!blend_rift_and_polygon && distance_to_L_polygon.first > 0. - 2. * sigma_polygon ? 1. : (1.0 - A_rift[2] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))));
+      std::vector<double> local_thicknesses = ic.compute_local_thicknesses(surface_position);
 
       // The local lithospheric column
       double local_rgh = 0;
@@ -204,9 +196,6 @@ namespace aspect
       {
         prm.enter_subsection("Lithosphere with rift");
         {
-          sigma_rift           = prm.get_double ("Standard deviation of Gaussian rift geometry");
-          sigma_polygon        = prm.get_double ("Half width of polygon smoothing");
-          blend_rift_and_polygon = prm.get_bool ("Blend polygons and rifts");
           A_rift = Utilities::possibly_extend_from_1_to_N(Utilities::string_to_double(Utilities::split_string_list(prm.get("Amplitude of Gaussian rift geometry"))),
                                                           3,
                                                           "Amplitude of Gaussian rift geometry");
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
index bc684324522..c44059dfa33 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
@@ -75,18 +75,6 @@ namespace aspect
         parse_parameters (ParameterHandler &prm) override;
 
       private:
-        /**
-         * The standard deviation of the rift-perpendicular Gaussian distribution
-         * of the thinning/thickening of the lithospheric thicknesses with its
-         * maximum along the rift axis.
-         */
-        double sigma_rift;
-
-        /**
-         * The half width of the hyperbolic tangent used to smooth the transitions
-         * between reference and polygon lithospheric thicknesses.
-         */
-        double sigma_polygon;
 
         /**
          * The maximum amplitude of the Gaussian distribution of the thinning/thickening
@@ -116,12 +104,6 @@ namespace aspect
          */
         double compensation_depth;
 
-        /**
-         * Whether or not to take the polygon thicknesses as dominant, or to smooth them
-         * gradually into rift areas.
-         */
-        bool blend_rift_and_polygon;
-
         /**
          * The maximum amplitude of the topography of the polygon area.
          */

From 734abde779043b897b28a47c65dd101f7ee0d9f6 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 31 May 2024 01:50:12 +0200
Subject: [PATCH 29/38] Indent

---
 .../doc/lithosphere_with_rift_IC_cookbook.md  | 16 +++++-----
 ...ns_continental_rift_initial_topography.prm |  8 ++---
 ...continental_rift_no_initial_topography.prm |  6 ++--
 .../lithosphere_rift_IC.cc                    |  8 ++---
 .../lithosphere_rift_IT_2.cc                  |  4 +--
 .../lithosphere_rift_topo.cc                  | 30 +++++++++----------
 6 files changed, 36 insertions(+), 36 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md b/cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md
index e92a6e347c7..08b4bd1893b 100644
--- a/cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md
+++ b/cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md
@@ -3,10 +3,10 @@
 *This section was contributed by Anne Glerum.*
 
 In order to localize deformation under prescribed far-field
-extension, initial weaknesses have to be introduced to the 
+extension, initial weaknesses have to be introduced to the
 model setup. Here we discuss plugins that 1) perturb the lithosphere
 consisting of upper crust, lower crust and mantle lithosphere
-at a user-specified location and 2) add initial plastic 
+at a user-specified location and 2) add initial plastic
 strain is around this same location. This strain represents
 inherited weakness for example from prior deformation phases.
 To represent other deviations of the reference lithosphere,
@@ -19,9 +19,9 @@ below. The temperature field is perturbed in the same way
 as the lithosphere compositional structure.
 
 In case the perturbations of the lithosphere in combination with
-the free surface induce large velocities initially, an initial 
+the free surface induce large velocities initially, an initial
 topography plugin approximates the topography resulting from
-isostatic equilibrium. 
+isostatic equilibrium.
 
 
 ## Initial lithosphere compositional fields and temperature
@@ -35,7 +35,7 @@ incipient rift and a cratonic region.
 
 The perturbation of the lithospheric layers that represents an
 incipient rift follows a Gaussian
-curve. We can either thicken or thin the layers, depending on 
+curve. We can either thicken or thin the layers, depending on
 the sign of the Gaussian amplitude: a negative amplitude thickens
 the corresponding layer and vice versa. The width of the perturbation
 is determined by the sigma of the Gaussian. The centre of the Gaussian
@@ -60,7 +60,7 @@ For the initial temperature we combine two plugins: one that prescribes
 a continental steady-state geotherm and one that computes an adiabatic
 temperature profile. The geotherm implementation is based on Chapter 4.6
 of Turcotte and Schubert. For each x-coordinate, it solves a steady-state
-heat conduction equation taking into account the respective densities, 
+heat conduction equation taking into account the respective densities,
 heat productivities and thermal conductivities of the three lithospheric
 layers. Below the lithospheric a NaN is returned, such that we can replace
 this NaN by an adiabatic temperature profile. Care has to be taken that the
@@ -78,7 +78,7 @@ adiabatic surface temperature matches the LAB temperature.
 ```
 
 To include inherited heterogeneity we also include initial plastic strain
-in the rift centre (Fig. {numref}`fig:initial_strain`). 
+in the rift centre (Fig. {numref}`fig:initial_strain`).
 We generate random strain values between 0 and 1 that
 are subsequently multiplied with a Gaussian distribution for which we specify
 the maximum amplitude and sigma. To control the depth extent of the initial
@@ -96,7 +96,7 @@ with a hyperbolic tangent.
 Sometimes the combination of a free surface with lateral variations in the
 lithospheric thicknesses leads to very high velocities in the first timesteps.
 To avoid a drunken sailor effect and/or very small timesteps, we can then
-prescribe initial topography that roughly fulfills isostatic equilibrium (Fig. {numref}`fig:initial_topography`). 
+prescribe initial topography that roughly fulfills isostatic equilibrium (Fig. {numref}`fig:initial_topography`).
 The required topography is computed using the reference density, so it neglects
 temperature effects on the density.
 
diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
index e662e023563..5e3f14b6e9d 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
@@ -40,7 +40,7 @@ subsection Geometry model
   # to obtain isostasy.
   subsection Initial topography model
     set Model name = lithosphere with rift
-  end 
+  end
 
 end
 
@@ -143,7 +143,7 @@ subsection Initial composition model
     set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
     # Where the rift axis should be. In this case in the centre of the domain.
     # In 3D simulations, line segments consisting of two coordinates
-    # should be provided. 
+    # should be provided.
     set Rift axis line segments                        = 200e3
 
     # The thicknesses of the lithospheric layer within a polygon
@@ -209,14 +209,14 @@ subsection Boundary temperature model
   subsection Box
     set Top temperature    =  293
     # Unrealistically high, so that it is always taken from initial temperature plugin
-    set Bottom temperature = 5000   
+    set Bottom temperature = 5000
   end
 end
 
 # Initial temperature field
 # The initial temperature consists of a typical continental geotherm
 # based on equations Turcotte and Schubert Ch. 4.6.
-# Below the lithosphere-asthenosphere boundary (LAB, defined initially by the 
+# Below the lithosphere-asthenosphere boundary (LAB, defined initially by the
 # bottom of the mantle lithsphere and the 1623 K isotherm,
 # we prescribe an adiabatic temperature increase.
 subsection Initial temperature model
diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
index 2472ad4884d..6bae84f1979 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
@@ -134,7 +134,7 @@ subsection Initial composition model
     set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
     # Where the rift axis should be. In this case in the centre of the domain.
     # In 3D simulations, line segments consisting of two coordinates
-    # should be provided. 
+    # should be provided.
     set Rift axis line segments                        = 200e3
 
     # The thicknesses of the lithospheric layer within a polygon
@@ -200,14 +200,14 @@ subsection Boundary temperature model
   subsection Box
     set Top temperature    =  293
     # Unrealistically high, so that it is always taken from initial temperature plugin
-    set Bottom temperature = 5000   
+    set Bottom temperature = 5000
   end
 end
 
 # Initial temperature field
 # The initial temperature consists of a typical continental geotherm
 # based on equations Turcotte and Schubert Ch. 4.6.
-# Below the lithosphere-asthenosphere boundary (LAB, defined initially by the 
+# Below the lithosphere-asthenosphere boundary (LAB, defined initially by the
 # bottom of the mantle lithsphere and the 1623 K isotherm,
 # we prescribe an adiabatic temperature increase.
 subsection Initial temperature model
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
index 38be60fe572..a929d933c4b 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IC.cc
@@ -178,13 +178,13 @@ namespace aspect
       // is smoothed by a hyperbolic tangent.
       const double polygon_contribution = (0.5 + 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon));
       const double rift_contribution = (0.5 - 0.5 * std::tanh(distance_to_L_polygon.first / sigma_polygon));
-      
+
       // The rift perturbation follows a Gaussian contribution.
       std::vector<double> local_thicknesses(3);
       for (unsigned int i = 0; i < 3; ++i)
-        local_thicknesses[i] = (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2))))) 
-        * reference_thicknesses[i] * rift_contribution + polygon_contribution * polygon_thicknesses[distance_to_L_polygon.second][i];
-      
+        local_thicknesses[i] = (1.0 - A_rift[i] * std::exp((-std::pow(distance_to_rift_axis, 2) / (2.0 * std::pow(sigma_rift, 2)))))
+                               * reference_thicknesses[i] * rift_contribution + polygon_contribution * polygon_thicknesses[distance_to_L_polygon.second][i];
+
       return local_thicknesses;
     }
 
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index dc644ac9a6d..7c2a4c6c866 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -75,8 +75,8 @@ namespace aspect
     initial_temperature (const Point<dim> &position) const
     {
       Assert(initial_composition_manager->template has_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>(),
-                  ExcMessage("The initial temperature plugin lithosphere with rift requires the corresponding initial composition plugin."));
-                  
+             ExcMessage("The initial temperature plugin lithosphere with rift requires the corresponding initial composition plugin."));
+
       // Get the initial composition plugin
       const InitialComposition::LithosphereRift<dim> &ic = initial_composition_manager->template get_matching_initial_composition_model<const InitialComposition::LithosphereRift<dim>>();
 
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
index dee6b5d1003..b13da041415 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.cc
@@ -101,28 +101,28 @@ namespace aspect
 
         }
 
-        // Make sure the compensation depth is in the sublithospheric mantle
-        compensation_depth = std::max(sum_thicknesses, std::max(sum_rift_thicknesses, max_sum_polygon_thicknesses)) + 5e3;
+      // Make sure the compensation depth is in the sublithospheric mantle
+      compensation_depth = std::max(sum_thicknesses, std::max(sum_rift_thicknesses, max_sum_polygon_thicknesses)) + 5e3;
 
-        // Add sublithospheric mantle part to the columns
-        ref_rgh += (compensation_depth - sum_thicknesses) * densities[0];
-        rift_rgh += (compensation_depth - sum_rift_thicknesses) * densities[0];
-        for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
+      // Add sublithospheric mantle part to the columns
+      ref_rgh += (compensation_depth - sum_thicknesses) * densities[0];
+      rift_rgh += (compensation_depth - sum_rift_thicknesses) * densities[0];
+      for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
         {
           polygon_rgh[i_polygons] += (compensation_depth - sum_polygon_thicknesses[i_polygons]) * densities[0];
         }
 
-        // Compute the maximum topography based on mass surplus/deficit
-        topo_rift_amplitude = (ref_rgh - rift_rgh) / densities[0];
-        for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
-          topo_polygon_amplitude = std::max((ref_rgh - polygon_rgh[i_polygons]) / densities[0], topo_polygon_amplitude);
+      // Compute the maximum topography based on mass surplus/deficit
+      topo_rift_amplitude = (ref_rgh - rift_rgh) / densities[0];
+      for (unsigned int i_polygons = 0; i_polygons < n_polygons; ++i_polygons)
+        topo_polygon_amplitude = std::max((ref_rgh - polygon_rgh[i_polygons]) / densities[0], topo_polygon_amplitude);
 
-        // TODO: probably there are combinations of rift and polygon topography
-        // that result in a higher topography
-        maximum_topography = std::max(topo_rift_amplitude, topo_polygon_amplitude);
+      // TODO: probably there are combinations of rift and polygon topography
+      // that result in a higher topography
+      maximum_topography = std::max(topo_rift_amplitude, topo_polygon_amplitude);
 
-        this->get_pcout() << "   Maximum initial topography of rift: " << topo_rift_amplitude << " m" << std::endl;
-        this->get_pcout() << "   Maximum initial topography of polygon: " << topo_polygon_amplitude << " m" << std::endl;
+      this->get_pcout() << "   Maximum initial topography of rift: " << topo_rift_amplitude << " m" << std::endl;
+      this->get_pcout() << "   Maximum initial topography of polygon: " << topo_polygon_amplitude << " m" << std::endl;
     }
 
 

From 4cb754aa408a44bb33ef31fb2655d5f62ef863ce Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 31 May 2024 01:54:54 +0200
Subject: [PATCH 30/38] Add cookbook to geophysical setups

---
 ...ift_IC_cookbook.md => initial_conditions_continental_rift.md} | 0
 doc/sphinx/user/cookbooks/geophysical-setups.md                  | 1 +
 2 files changed, 1 insertion(+)
 rename cookbooks/initial_conditions_continental_rift/doc/{lithosphere_with_rift_IC_cookbook.md => initial_conditions_continental_rift.md} (100%)

diff --git a/cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md b/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
similarity index 100%
rename from cookbooks/initial_conditions_continental_rift/doc/lithosphere_with_rift_IC_cookbook.md
rename to cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
diff --git a/doc/sphinx/user/cookbooks/geophysical-setups.md b/doc/sphinx/user/cookbooks/geophysical-setups.md
index 6146b3d9cfc..bf113543c55 100644
--- a/doc/sphinx/user/cookbooks/geophysical-setups.md
+++ b/doc/sphinx/user/cookbooks/geophysical-setups.md
@@ -102,6 +102,7 @@ cookbooks/multicomponent_steinberger/doc/multicomponent_steinberger.md
 cookbooks/morency_doin_2004/doc/morency_doin_2004.md
 cookbooks/crustal_deformation/doc/crustal_deformation.md
 cookbooks/continental_extension/doc/continental_extension.md
+cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
 cookbooks/inner_core_convection/doc/inner_core_convection.md
 cookbooks/lower_crustal_flow/doc/lower_crustal_flow.md
 cookbooks/global_melt/doc/global_melt.md

From 7c1f59f6eb29c6a10b7b617e64385e46c27e2a5b Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 31 May 2024 03:49:11 +0200
Subject: [PATCH 31/38] Fix typos and md syntax

---
 .../doc/initial_conditions_continental_rift.md               | 5 ++---
 .../lithosphere_rift_topo.h                                  | 2 +-
 2 files changed, 3 insertions(+), 4 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md b/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
index 08b4bd1893b..8ed3c337dcd 100644
--- a/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
+++ b/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
@@ -49,7 +49,7 @@ In addition to a rift centre, other deviations from the reference
 lithospheric thicknesses can also be prescribed. In the above snippet,
 these are specified as polygons (multiple polygons are allowed) with
 their own layer thicknesses. The transition from reference lithosphere
-to polgyon lithosphere is implemented as a hyperbolic tangent with a
+to polygon lithosphere is implemented as a hyperbolic tangent with a
 centre point and a half-width.
 
 
@@ -70,8 +70,6 @@ adiabatic surface temperature matches the LAB temperature.
 <img src="Initial_temperature_with_craton.*" style="width:60.0%" />
 
  The initial temperature distribution.
-
-```{literalinclude} initial_topography.prm
 ```
 
 ```{literalinclude} initial_composition_strain.prm
@@ -89,6 +87,7 @@ with a hyperbolic tangent.
 <img src="Initial_strain_with_craton.*" style="width:60.0%" />
 
  The initial plastic strain distribution.
+```
 
 ```{literalinclude} initial_topography.prm
 ```
diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
index c44059dfa33..7020543fd8f 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_topo.h
@@ -93,7 +93,7 @@ namespace aspect
         double topo_rift_amplitude;
 
         /**
-         * The product of density, gravitational accelleration constant and thickness of the
+         * The product of density, gravitational acceleration constant and thickness of the
          * reference lithospheric column used in computing the topography based on isostasy.
          */
         double ref_rgh;

From 69de1044a6375e8a818c68bbc165231ede458360 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 31 May 2024 04:23:25 +0200
Subject: [PATCH 32/38] Add prm snippets and fix figure name

---
 .../doc/initial_composition_lithosphere.prm   | 59 +++++++++++++++++++
 .../doc/initial_composition_strain.prm        | 22 +++++++
 .../initial_conditions_continental_rift.md    |  2 +-
 .../doc/initial_temperature.prm               | 45 ++++++++++++++
 .../doc/initial_topography.prm                | 19 ++++++
 5 files changed, 146 insertions(+), 1 deletion(-)
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/initial_composition_lithosphere.prm
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/initial_composition_strain.prm
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/initial_temperature.prm
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/initial_topography.prm

diff --git a/cookbooks/initial_conditions_continental_rift/doc/initial_composition_lithosphere.prm b/cookbooks/initial_conditions_continental_rift/doc/initial_composition_lithosphere.prm
new file mode 100644
index 00000000000..a34ad95ed99
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/doc/initial_composition_lithosphere.prm
@@ -0,0 +1,59 @@
+# Number and names of compositional fields
+# The five compositional fields represent:
+# 1. The plastic strain that accumualates over time, with the initial plastic strain removed
+# 2. The plastic strain that accumulated over time, including the initial plastic strain values
+# 3. The upper crust
+# 4. The lower crust
+# 5. The mantle lithosphere
+subsection Compositional fields
+  set Number of fields = 5
+  set Names of fields = noninitial_plastic_strain, plastic_strain, upper, lower, mantle_L
+end
+
+# Initial values of different compositional fields
+# The upper crust (20 km thick), lower crust (15 km thick)
+# and mantle (85 km thick) are continuous horizontal layers
+# of constant thickness, except in a center area.
+# In the centre of the domain, the upper crust is thickened to 25 km,
+# while the mantle lithosphere is thinned. The transition from this
+# perturbed center to the reference thicknesses of the lithospheric
+# layers is smoothened using a Gaussian. The combined effect
+# is a hotter, weaker centre area that localizes deformation.
+# An additional thicker/stronger area is added on the right of the domain
+# to represent cratonic lithosphere. The transition in layer thicknesses
+# uses a hyperbolic tangent.
+# The non initial plastic strain is set
+# to 0 and the initial plastic strain is randomized between
+# 0.5 and 1.5 in an area around the rift axis.
+subsection Initial composition model
+  set List of model names = lithosphere with rift, rift box initial plastic strain, function
+
+  subsection Lithosphere with rift
+    # The reference layer thicknesses of the upper crust, lower crust and mantle lithosphere.
+    set Layer thicknesses                              = 20e3, 15e3, 85e3
+    # How wide the weak zone will be
+    set Standard deviation of Gaussian rift geometry   = 50e3
+    # The maximum thinning/thickening of the lithospheric layers
+    set Amplitude of Gaussian rift geometry            = -0.25, 0, 0.17647
+    # Where the rift axis should be. In this case in the centre of the domain.
+    # In 3D simulations, line segments consisting of two coordinates
+    # should be provided.
+    set Rift axis line segments                        = 200e3
+
+    # The thicknesses of the lithospheric layer within a polygon
+    set Lithospheric polygon layer thicknesses         = 20e3, 15e3 , 115.e3
+    # The segments making up the polygon
+    set Lithospheric polygons                          = 550e3 > 3000e3
+    # The half width of the transition from polygon to reference lithosphere
+    set Half width of polygon smoothing                = 10e3
+  end
+
+  subsection Function
+    set Variable names = x,y
+    set Function expression = 0; \
+                              0; \
+                              0; \
+                              0; \
+                              0
+  end
+end
diff --git a/cookbooks/initial_conditions_continental_rift/doc/initial_composition_strain.prm b/cookbooks/initial_conditions_continental_rift/doc/initial_composition_strain.prm
new file mode 100644
index 00000000000..e56717798f2
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/doc/initial_composition_strain.prm
@@ -0,0 +1,22 @@
+subsection Initial composition model
+  set List of model names = lithosphere with rift, rift box initial plastic strain, function
+
+  # Inherited plastic strain
+  subsection Rift box initial plastic strain
+    # We focus initial strain around the rift axis
+    set Rift axis line segments                                         = 200e3
+    # The strain values follow a Gaussian distribution around the rift axis
+    # The maximum magnitude of the strain
+    set Maximum amplitude of Gaussian noise amplitude distribution      = 0.250000
+    # The sigma width of the area of strain
+    set Standard deviation of Gaussian noise amplitude distribution     = 50e3
+    # The number with which to start of the random number generator
+    set Random number generator seed                                    = 2
+    # Using a hyperbolic tangent centred around this value,
+    # we smooth out the strain with increasing depth.
+    set Depth around which Gaussian noise is smoothed out               = 50e3
+    # The halfwidth of the hyperbolic tangent.
+    set Halfwidth with which Gaussian noise is smoothed out in depth    = 10e3
+  end
+
+end
diff --git a/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md b/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
index 8ed3c337dcd..90bd8685f7d 100644
--- a/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
+++ b/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
@@ -84,7 +84,7 @@ strain, we specify a depth around which the amplitude is smoothed to zero
 with a hyperbolic tangent.
 
 ```{figure-md} fig:initial_strain
-<img src="Initial_strain_with_craton.*" style="width:60.0%" />
+<img src="Initial_plastic_strain_with_craton.*" style="width:60.0%" />
 
  The initial plastic strain distribution.
 ```
diff --git a/cookbooks/initial_conditions_continental_rift/doc/initial_temperature.prm b/cookbooks/initial_conditions_continental_rift/doc/initial_temperature.prm
new file mode 100644
index 00000000000..3413cac7c47
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/doc/initial_temperature.prm
@@ -0,0 +1,45 @@
+# Temperature boundary conditions
+# Top and bottom (fixed) temperatures are consistent with the initial temperature field.
+# Because we use a free surface, the height/depth of the surface can change over time,
+# meaning that if the initial temperature plugin is asked for the temperature
+# at the surface, this temperature could also vary over time. Therefore
+# we also use the box plugin and take the minimum of the initial temperature and
+# the box plugins, thus maintaining a temperature of 293 K.
+subsection Boundary temperature model
+  set Fixed temperature boundary indicators   = bottom, top
+  set List of model names = initial temperature, box
+  set List of model operators = add, minimum
+  subsection Box
+    set Top temperature    =  293
+    # Unrealistically high, so that it is always taken from initial temperature plugin
+    set Bottom temperature = 5000
+  end
+end
+
+# Initial temperature field
+# The initial temperature consists of a typical continental geotherm
+# based on equations Turcotte and Schubert Ch. 4.6.
+# Below the lithosphere-asthenosphere boundary (LAB, defined initially by the
+# bottom of the mantle lithsphere and the 1623 K isotherm,
+# we prescribe an adiabatic temperature increase.
+subsection Initial temperature model
+  set List of model names = adiabatic, lithosphere with rift
+  set List of model operators = add, replace if valid
+  subsection Lithosphere with rift
+    set LAB isotherm temperature = 1573.
+    set Surface temperature = 293.
+  end
+  subsection Adiabatic
+    # A reference profile of the compositional fields
+    # where x represents depth
+    subsection Function
+    # noninitial_plastic_strain, plastic_strain, upper, lower, mantle_L
+    set Function expression           = 0; \
+                                        0; \
+                                        if(x<20e3,1,0); \
+                                        if(x>=20e3&x<35e3,1,0); \
+                                        if(x>=35e3&x<120e3,1,0)
+    end
+  end
+
+end
diff --git a/cookbooks/initial_conditions_continental_rift/doc/initial_topography.prm b/cookbooks/initial_conditions_continental_rift/doc/initial_topography.prm
new file mode 100644
index 00000000000..34ef795c2e9
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/doc/initial_topography.prm
@@ -0,0 +1,19 @@
+# Model geometry (400x200 km, 40 km spacing)
+subsection Geometry model
+  set Model name = box
+
+  subsection Box
+    set X repetitions = 10
+    set Y repetitions = 5
+    set X extent      = 400e3
+    set Y extent      = 200e3
+  end
+
+  # With respect to the reference lithosphere,
+  # move the surface of perturbed lithosphere
+  # to obtain isostasy.
+  subsection Initial topography model
+    set Model name = lithosphere with rift
+  end
+
+end

From dbb32762653adeb36c050c33957c47e0ae27d010 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Mon, 17 Jun 2024 15:02:58 +0200
Subject: [PATCH 33/38] Expand description, add boundary conditions

---
 .../initial_conditions_continental_rift.md    | 128 ++++++++++++------
 .../doc/initial_temperature.prm               |   5 +
 .../doc/velocity_boundary_conditions.prm      |  28 ++++
 3 files changed, 122 insertions(+), 39 deletions(-)
 create mode 100644 cookbooks/initial_conditions_continental_rift/doc/velocity_boundary_conditions.prm

diff --git a/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md b/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
index 90bd8685f7d..70b45591b9e 100644
--- a/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
+++ b/cookbooks/initial_conditions_continental_rift/doc/initial_conditions_continental_rift.md
@@ -1,30 +1,42 @@
-# Initial conditions for continental rifting
+# Initial and boundary conditions for continental rifting
 
 *This section was contributed by Anne Glerum.*
 
-In order to localize deformation under prescribed far-field
-extension, initial weaknesses have to be introduced to the
-model setup. Here we discuss plugins that 1) perturb the lithosphere
-consisting of upper crust, lower crust and mantle lithosphere
-at a user-specified location and 2) add initial plastic
-strain is around this same location. This strain represents
-inherited weakness for example from prior deformation phases.
+Continental rifting is a process that thins the continental
+lithosphere and can eventually lead to full break-up of that lithosphere
+and seafloor spreading at a mid-ocean ridge {cite}[e.g., ][]`brune:2023`.
+We can simulate continental rifting under far-field extensional
+forces by prescribing certain velocities or stresses on the lateral
+boundaries of our model domain (as in, for example, section 
+{ref}`sec:cookbooks:continental_extension`).
+Here we choose to prescribe outward horizontal velocities on
+the lateral boundaries.
+In order to localize deformation under this prescribed 
+extension (and avoid localizing at the model boundaries), 
+we have to introduce initial weaknesses to the
+model setup. The plugins prescribed in this cookbook set up
+a lithospheric (upper crust, lower crust and mantle lithosphere) and asthenosphere
+composition and temperature structure and then
+add weaknesses by 1) smoothly perturbing the lithosphere
+at user-specified locations and by 2) adding initial plastic
+strain around these same locations. This strain represents
+inherited weakness from for example prior deformation phases.
 To represent other deviations of the reference lithosphere,
+such as cratonic lithosphere, 
 additional regions of different lithospheric layer thicknesses
-can also be specified.
-
-The initial temperature plugin prescribes a steady-state
-continental geotherm within the lithosphere and an adiabat
-below. The temperature field is perturbed in the same way
-as the lithosphere compositional structure.
-
+can be specified.
 In case the perturbations of the lithosphere in combination with
-the free surface induce large velocities initially, an initial
-topography plugin approximates the topography resulting from
-isostatic equilibrium.
+a free surface or another type of mesh deformation induce large initial 
+velocities, an initial topography plugin approximates the topography resulting from
+isostatic equilibrium with respect to the reference (unperturbed) lithosphere.
 
+Apart from prescribing tensional velocities on the lateral boundaries of
+the box domain, we use the surface processes software FastScape to
+modify the top boundary and a traction boundary condition for the bottom
+boundary. This allows for the inclusion of sediment erosion, transport
+and deposition, and the automatic balance of mass within the model domain.
 
-## Initial lithosphere compositional fields and temperature
+## Initial lithosphere composition and temperature
 
 ```{figure-md} fig:setup
 <img src="Initial_density_with_craton.*" style="width:80.0%" />
@@ -32,56 +44,72 @@ isostatic equilibrium.
 Lithospheric structure with perturbations that represent an
 incipient rift and a cratonic region.
 ```
-
-The perturbation of the lithospheric layers that represents an
-incipient rift follows a Gaussian
-curve. We can either thicken or thin the layers, depending on
-the sign of the Gaussian amplitude: a negative amplitude thickens
+To set up the reference lithospheric structure, we specify the Layer thicknesses
+of the upper crust, lower crust and mantle lithosphere within the Lithosphere with rift 
+subsection (see input-file snippet below). The perturbations of these lithospheric layers - representing an
+incipient rift and localizing deformation - follow Gaussian curves. 
+We can either thicken or thin the layers, depending on
+the sign of each Gaussian amplitude specified: a negative amplitude thickens
 the corresponding layer and vice versa. The width of the perturbation
-is determined by the sigma of the Gaussian. The centre of the Gaussian
-curve will be the rift centre. The parameters that need to be set are:
+is determined by the sigma of the Gaussians. The centre of the Gaussian
+curve will be the rift centre and is set with the parameter Rift axis line segments: 
 
 
 ```{literalinclude} initial_composition_lithosphere.prm
 ```
 
-In addition to a rift centre, other deviations from the reference
-lithospheric thicknesses can also be prescribed. In the above snippet,
+Note that you can specify multiple segments, both in 2D and in 3D. By changing
+the thickness of the layers, we simultaneously change the temperature profile,
+and thus the strength distribution, creating weaker lithosphere.
+
+In addition to an incipient rift, other deviations from the reference
+lithospheric thicknesses can also be prescribed (e.g., representing thick, cold cratonic
+lithosphere). In the above snippet,
 these are specified as polygons (multiple polygons are allowed) with
 their own layer thicknesses. The transition from reference lithosphere
 to polygon lithosphere is implemented as a hyperbolic tangent with a
-centre point and a half-width.
+centre point defined by the coordinates of the polygon and a half-width (10 km in this case).
 
 
 ```{literalinclude} initial_temperature.prm
 ```
 
+
 For the initial temperature we combine two plugins: one that prescribes
-a continental steady-state geotherm and one that computes an adiabatic
-temperature profile. The geotherm implementation is based on Chapter 4.6
+a continental steady-state geotherm (lithosphere with rift) and one that computes an adiabatic
+temperature profile (see snippet above). The geotherm implementation is based on Chapter 4.6
 of Turcotte and Schubert. For each x-coordinate, it solves a steady-state
 heat conduction equation taking into account the respective densities,
 heat productivities and thermal conductivities of the three lithospheric
-layers. Below the lithospheric a NaN is returned, such that we can replace
-this NaN by an adiabatic temperature profile. Care has to be taken that the
-adiabatic surface temperature matches the LAB temperature.
+layers and the user-set temperature at the top (Surface temperature) and 
+bottom of the lithosphere (LAB isotherm temperature). Below the lithosphere a NaN is returned, such that we can replace
+this NaN by an adiabatic temperature profile. Care has to be taken to match
+the user-specified LAB temperature and the adiabatic temperature at the same
+depth by modifying the adiabatic surface temperature. One can choose to prescribe
+the LAB temperature up to a certain compensation depth (e.g., the bottom of the
+craton), such that the LAB and adiabatic temperatures match everywhere (Fig. {numref}`fig:initial_temperature`).
 
 ```{figure-md} fig:initial_temperature
 <img src="Initial_temperature_with_craton.*" style="width:60.0%" />
 
  The initial temperature distribution.
 ```
+## Inherited heterogeneity
 
 ```{literalinclude} initial_composition_strain.prm
 ```
 
 To include inherited heterogeneity we also include initial plastic strain
-in the rift centre (Fig. {numref}`fig:initial_strain`).
+around the rift centre (Fig. {numref}`fig:initial_strain`). This requires a
+compositional field called plastic_strain and the plugin rift box initial plastic strain.
 We generate random strain values between 0 and 1 that
 are subsequently multiplied with a Gaussian distribution for which we specify
 the maximum amplitude and sigma. To control the depth extent of the initial
-strain, we specify a depth around which the amplitude is smoothed to zero
-with a hyperbolic tangent.
+strain, we specify a depth around which the amplitude is smoothed out to zero
+with a hyperbolic tangent. The initial strain thus produced will be the same
+for each run with the same specifications if the same number of MPI processes is used.
+The plastic strain can be used to weaken the cohesion and/or internal angle of friction
+of the plastic rheology, thus again providing weaknesses that localize deformation.
 
 ```{figure-md} fig:initial_strain
 <img src="Initial_plastic_strain_with_craton.*" style="width:60.0%" />
@@ -92,12 +120,14 @@ with a hyperbolic tangent.
 ```{literalinclude} initial_topography.prm
 ```
 
+## Initial topography
+
 Sometimes the combination of a free surface with lateral variations in the
 lithospheric thicknesses leads to very high velocities in the first timesteps.
 To avoid a drunken sailor effect and/or very small timesteps, we can then
 prescribe initial topography that roughly fulfills isostatic equilibrium (Fig. {numref}`fig:initial_topography`).
-The required topography is computed using the reference density, so it neglects
-temperature effects on the density.
+The required topography is computed using the reference density for each material, 
+so it neglects temperature effects on the density.
 
 
 ```{figure-md} fig:initial_topography
@@ -106,3 +136,23 @@ temperature effects on the density.
  The initial topography that roughly isostatically balances the rift perturbation and craton region
  with respect to the reference lithosphere.
 ```
+
+## Boundary conditions
+
+```{literalinclude} velocity_boundary_conditions.prm
+```
+Extension is driven by outward horizontal velocities on the left and
+right boundary of the model domain. To compensate for this outflow,
+we open the bottom boundary to flow by prescribing a traction. The 
+prescribed traction is computed as the initial lithostatic pressure 
+at a user-specified point. We pick this point to lie in the reference
+(unperturbed) lithosphere close to the left domain boundary.
+
+For the top boundary, we pick the mesh deformation plugin fastscape,
+which provides an interface to the FastScape landscape evolution model.
+This plugin computes changes to the mesh's surface topography based on
+river incision, hill slope diffusion, sediment deposition and marine diffusion. 
+For all the different parameters relating to FastScape, have a look at 
+section {ref}`sec:cookbooks:fastscape_eroding_box`. We allow the top corner
+of the right boundary to move with the surface, but not the left top corner point,
+as this is our reference location.
diff --git a/cookbooks/initial_conditions_continental_rift/doc/initial_temperature.prm b/cookbooks/initial_conditions_continental_rift/doc/initial_temperature.prm
index 3413cac7c47..26b74f5a00d 100644
--- a/cookbooks/initial_conditions_continental_rift/doc/initial_temperature.prm
+++ b/cookbooks/initial_conditions_continental_rift/doc/initial_temperature.prm
@@ -28,6 +28,11 @@ subsection Initial temperature model
   subsection Lithosphere with rift
     set LAB isotherm temperature = 1573.
     set Surface temperature = 293.
+    # Whether or not to prescribe the LAB temperature up to a
+    # certain depth (in the area below LAB)
+    # or to use adiabat everywhere below the LAB.
+    set Use temperature compensation depth = true
+    set Temperature compensation depth = 150e3
   end
   subsection Adiabatic
     # A reference profile of the compositional fields
diff --git a/cookbooks/initial_conditions_continental_rift/doc/velocity_boundary_conditions.prm b/cookbooks/initial_conditions_continental_rift/doc/velocity_boundary_conditions.prm
new file mode 100644
index 00000000000..20babcfbe8d
--- /dev/null
+++ b/cookbooks/initial_conditions_continental_rift/doc/velocity_boundary_conditions.prm
@@ -0,0 +1,28 @@
+subsection Boundary velocity model
+  set Prescribed velocity boundary indicators = left: function, right: function
+  set Tangential velocity boundary indicators =
+  subsection Function
+    set Coordinate system   = cartesian
+    set Variable names      = x,y,t
+    set Function constants  = mm=0.001, yr=1, Z=300e3, X=700e3, outflow=10
+    set Function expression = if(x<X/2,-1,1)*outflow/2*mm/yr; \
+                              0   
+  end 
+end
+
+subsection Boundary traction model
+  set Prescribed traction boundary indicators = bottom: initial lithostatic pressure
+  subsection Initial lithostatic pressure
+    set Representative point = 10000,0
+  end 
+end
+
+subsection Mesh deformation
+  set Additional tangential mesh velocity boundary indicators = right
+  set Mesh deformation boundary indicators = top: fastscape
+  set Surface stabilization theta = 1.0 
+
+  subsection Fastscape
+  ...
+  end
+end

From 0fc48aef5db00ffcc75099f19ebe9112ee02c864 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Tue, 18 Jun 2024 10:51:16 +0200
Subject: [PATCH 34/38] Add FS and traction BC

---
 ...ns_continental_rift_initial_topography.prm | 74 +++++++++++++++----
 1 file changed, 59 insertions(+), 15 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
index 5e3f14b6e9d..a29240a61cb 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
@@ -1,18 +1,19 @@
 #### This is an adaptation of the Continental Extension Cookbook
-#### using new plugins for the initial composition, temperature
-#### topography and strain of an incipient continental rift system.
+#### using new plugins for the initial composition, temperature, 
+#### topography and initial strain of an incipient continental rift system.
+#### Additionally, we use FastScape and traction boundary condition.
 
 ####  Global parameters
 set Additional shared libraries            = $ASPECT_SOURCE_DIR/cookbooks/initial_conditions_continental_rift/libinitial_conditions_continental_rift.debug.so
 set Dimension                              = 2
 set Start time                             = 0
-set End time                               = 0 #5e6
+set End time                               = 5e6
 set Use years in output instead of seconds = true
 set Nonlinear solver scheme                = single Advection, iterated Stokes
 set Nonlinear solver tolerance             = 1e-5
 set Max nonlinear iterations               = 2
 set CFL number                             = 0.5
-set Maximum time step                      = 20e3
+set Maximum time step                      = 5000 
 set Output directory                       = output-initial_conditions_continental_rift_initial_topography_with_craton
 set Pressure normalization                 = no
 set Adiabatic surface temperature          = 1573
@@ -70,22 +71,65 @@ subsection Solver parameters
   end
 end
 
-# Advecting the free surface using a normal, rather than vertical,
-# projection. To reduce mesh instabilities and associated solver
-# issues when deformation becomes large, diffusion is applied to
-# the free surface at each time step.
+# Use FastScape to deform the mesh.
 subsection Mesh deformation
-  set Mesh deformation boundary indicators        = top: free surface, top: diffusion
+  set Additional tangential mesh velocity boundary indicators = right
+  set Mesh deformation boundary indicators = top: fastscape
 
   subsection Free surface
-    set Surface velocity projection = normal
+    set Free surface stabilization theta = 1
   end
+  
+  subsection Fastscape
+    set Vertical exaggeration = -1
+    set Maximum timestep length = 500
+    set Number of fastscape timesteps per aspect timestep = 10
+    set Maximum surface refinement level = 4
+    set Surface refinement difference = 0
+    set Additional fastscape refinement = 0
+    set Use ghost nodes = true
+    set Y extent in 2d = 25e3
+    set Uplift and advect with fastscape = true
+
+    subsection Boundary conditions
+      set Front = 1
+      set Right = 1
+      set Back  = 1
+      set Left  = 1
+    end
+
+    subsection Erosional parameters
+      set Drainage area exponent = 0.4              #m
+      set Slope exponent = 1                        #n
+      set Multi-direction slope exponent = -1        #p
+
+      set Bedrock diffusivity = 5e-3          #kd
+      set Bedrock river incision rate = 1e-5        #kf
+      set Bedrock deposition coefficient = 1       #G
 
-  subsection Diffusion
-    # Diffusivity term. Increasing this value will result
-    # in a smoother free surface and lower topography
-    # amplitudes.
-    set Hillslope transport coefficient = 1.e-8
+      set Sediment diffusivity = -1
+      set Sediment river incision rate = -1
+      set Sediment deposition coefficient = 1        #G
+    end
+
+    set Use marine component = true
+    set Sediment rain rates = 1e-4 # m/yr
+    set Sediment rain intervals =
+    set Use stratigraphy   = false
+
+    # No difference between sand and silt
+    subsection Marine parameters
+      set Sea level = -200
+      set Sand porosity = 0.
+      set Silt porosity = 0.
+      set Sand e-folding depth = 3000 # m
+      set Silt e-folding depth = 3000 # m
+
+      set Sand-silt ratio = 0.5
+      set Depth averaging thickness = 1e3 # m
+      set Sand transport coefficient = 150 # m2/yr
+      set Silt transport coefficient = 150 # m2/yr
+    end
   end
 end
 

From d16bcaee9c7dfea07a14abf0bdba6e48f56b12ae Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 20 Jun 2024 09:32:21 +0200
Subject: [PATCH 35/38] Rm screen output

---
 .../rift_box_initial_plastic_strain.cc                        | 4 ----
 1 file changed, 4 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
index 4749c0e9752..59624a6b47f 100644
--- a/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
+++ b/cookbooks/initial_conditions_continental_rift/rift_box_initial_plastic_strain.cc
@@ -247,10 +247,6 @@ namespace aspect
       // to cover 10 km at the same resolution. Round up the number of cells.
       grid_intervals[dim-1] += static_cast<int>(std::ceil(maximum_initial_topography / (extents[dim-1] / grid_intervals[dim-1])));
 
-      this->get_pcout() << "Max initial topo: " << maximum_initial_topography << std::endl;
-      this->get_pcout() << "Grid intervals X: " << grid_intervals[0] << std::endl;
-      this->get_pcout() << "Grid intervals Y: " << grid_intervals[dim-1] << std::endl;
-
       prm.enter_subsection("Initial composition model");
       {
         prm.enter_subsection("Rift box initial plastic strain");

From 70f1e8f818e59e9fc50dbeb57c564e96ba827687 Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 20 Jun 2024 09:33:54 +0200
Subject: [PATCH 36/38] Use FastScape instead of free surface

---
 ...ns_continental_rift_initial_topography.prm |  3 +-
 ...continental_rift_no_initial_topography.prm | 65 +++++++++++++++----
 2 files changed, 55 insertions(+), 13 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
index a29240a61cb..018aae8dde1 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
@@ -114,8 +114,7 @@ subsection Mesh deformation
 
     set Use marine component = true
     set Sediment rain rates = 1e-4 # m/yr
-    set Sediment rain intervals =
-    set Use stratigraphy   = false
+    set Sediment rain time intervals =
 
     # No difference between sand and silt
     subsection Marine parameters
diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
index 6bae84f1979..33007a01a4f 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_no_initial_topography.prm
@@ -61,22 +61,65 @@ subsection Solver parameters
   end
 end
 
-# Advecting the free surface using a normal, rather than vertical,
-# projection. To reduce mesh instabilities and associated solver
-# issues when deformation becomes large, diffusion is applied to
-# the free surface at each time step.
+
+# Use FastScape to deform the mesh.
 subsection Mesh deformation
-  set Mesh deformation boundary indicators        = top: free surface, top: diffusion
+  set Additional tangential mesh velocity boundary indicators = right
+  set Mesh deformation boundary indicators = top: fastscape
 
   subsection Free surface
-    set Surface velocity projection = normal
+    set Free surface stabilization theta = 1
   end
+  
+  subsection Fastscape
+    set Vertical exaggeration = -1
+    set Maximum timestep length = 500
+    set Number of fastscape timesteps per aspect timestep = 10
+    set Maximum surface refinement level = 4
+    set Surface refinement difference = 0
+    set Additional fastscape refinement = 0
+    set Use ghost nodes = true
+    set Y extent in 2d = 25e3
+    set Uplift and advect with fastscape = true
+
+    subsection Boundary conditions
+      set Front = 1
+      set Right = 1
+      set Back  = 1
+      set Left  = 1
+    end
+
+    subsection Erosional parameters
+      set Drainage area exponent = 0.4              #m
+      set Slope exponent = 1                        #n
+      set Multi-direction slope exponent = -1        #p
+
+      set Bedrock diffusivity = 5e-3          #kd
+      set Bedrock river incision rate = 1e-5        #kf
+      set Bedrock deposition coefficient = 1       #G
 
-  subsection Diffusion
-    # Diffusivity term. Increasing this value will result
-    # in a smoother free surface and lower topography
-    # amplitudes.
-    set Hillslope transport coefficient = 1.e-8
+      set Sediment diffusivity = -1
+      set Sediment river incision rate = -1
+      set Sediment deposition coefficient = 1        #G
+    end
+
+    set Use marine component = true
+    set Sediment rain rates = 1e-4 # m/yr
+    set Sediment rain time intervals =
+
+    # No difference between sand and silt
+    subsection Marine parameters
+      set Sea level = -200
+      set Sand porosity = 0.
+      set Silt porosity = 0.
+      set Sand e-folding depth = 3000 # m
+      set Silt e-folding depth = 3000 # m
+
+      set Sand-silt ratio = 0.5
+      set Depth averaging thickness = 1e3 # m
+      set Sand transport coefficient = 150 # m2/yr
+      set Silt transport coefficient = 150 # m2/yr
+    end
   end
 end
 

From 8ab8bf18df7d1c125d9baf4ec03ae1fc655b22fa Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Thu, 4 Jul 2024 17:13:35 +0200
Subject: [PATCH 37/38] Use traction bottom BC

---
 .../doc/velocity_boundary_conditions.prm              |  1 -
 ...conditions_continental_rift_initial_topography.prm | 11 +++++++++--
 2 files changed, 9 insertions(+), 3 deletions(-)

diff --git a/cookbooks/initial_conditions_continental_rift/doc/velocity_boundary_conditions.prm b/cookbooks/initial_conditions_continental_rift/doc/velocity_boundary_conditions.prm
index 20babcfbe8d..826efdc814f 100644
--- a/cookbooks/initial_conditions_continental_rift/doc/velocity_boundary_conditions.prm
+++ b/cookbooks/initial_conditions_continental_rift/doc/velocity_boundary_conditions.prm
@@ -20,7 +20,6 @@ end
 subsection Mesh deformation
   set Additional tangential mesh velocity boundary indicators = right
   set Mesh deformation boundary indicators = top: fastscape
-  set Surface stabilization theta = 1.0 
 
   subsection Fastscape
   ...
diff --git a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
index 018aae8dde1..44801740206 100644
--- a/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
+++ b/cookbooks/initial_conditions_continental_rift/initial_conditions_continental_rift_initial_topography.prm
@@ -138,12 +138,19 @@ end
 # Velocity components parallel to the base (x-velocity) and side walls (y-velocity)
 # are unconstrained (i.e. 'free').
 subsection Boundary velocity model
-  set Prescribed velocity boundary indicators = left x: function, right x:function, bottom y:function
+  set Prescribed velocity boundary indicators = left: function, right:function
 
   subsection Function
     set Variable names      = x,y
     set Function constants  = v=0.0025, w=200.e3, d=100.e3
-    set Function expression = if (x < w/2 , -v, v) ; v*2*d/w
+    set Function expression = if (x < w/2 , -v, v) ; 0
+  end
+end
+
+subsection Boundary traction model
+  set Prescribed traction boundary indicators = bottom: initial lithostatic pressure
+  subsection Initial lithostatic pressure
+    set Representative point = 10000,0
   end
 end
 

From cb4758d6a237429dfe07c1001a882170ba5f09df Mon Sep 17 00:00:00 2001
From: anne-glerum <a.c.glerum@uu.nl>
Date: Fri, 4 Oct 2024 16:49:17 +0200
Subject: [PATCH 38/38] Fix typo

---
 .../lithosphere_rift_IT_2.cc                                    | 2 +-
 1 file changed, 1 insertion(+), 1 deletion(-)

diff --git a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
index 7c2a4c6c866..38cf202c95d 100644
--- a/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
+++ b/cookbooks/initial_conditions_continental_rift/lithosphere_rift_IT_2.cc
@@ -273,7 +273,7 @@ namespace aspect
 
           // To obtain the radioactive heating rate in W/kg, we divide the volumetric heating rate by density
           AssertThrow(heat_productivities.size() == 3 && densities.size() == 3 && conductivities.size() == 3,
-                      ExcMessage("The entries for density, conductivity and heat production do not match with the expected number of layers (3)."))
+                      ExcMessage("The entries for density, conductivity and heat production do not match with the expected number of layers (3)."));
 
           for (unsigned int i = 0; i<3; ++i)
             heat_productivities[i] /= densities[i];