[cig-commits] [commit] devel, master: renames the USE_RICKER_IPATI flag in USE_RICKER_TIME_FUNCTION and moves it from constants.h.in to the Par_file (6d74f14)
cig_noreply at geodynamics.org
cig_noreply at geodynamics.org
Wed Jun 18 16:49:57 PDT 2014
Repository : https://github.com/geodynamics/specfem3d
On branches: devel,master
Link : https://github.com/geodynamics/specfem3d/compare/6026e367984905ab133865f62fa6293b343759b9...47f703851338234f96397e7da9fbff63d8178b8a
>---------------------------------------------------------------
commit 6d74f14d131e00f70d379f6c0ed5d93d612739b6
Author: Joseph Charles <jcharles at lma.cnrs-mrs.fr>
Date: Fri Oct 19 14:07:15 2012 +0000
renames the USE_RICKER_IPATI flag in USE_RICKER_TIME_FUNCTION and moves it from constants.h.in to the Par_file
>---------------------------------------------------------------
6d74f14d131e00f70d379f6c0ed5d93d612739b6
BENCHMARK_CLAERBOUT_ADJOINT/ACOUSTIC/in_data_files/Par_file | 4 ++++
BENCHMARK_CLAERBOUT_ADJOINT/ELASTIC/in_data_files/Par_file | 4 ++++
Mount_StHelens/in_data_files/Par_file | 4 ++++
homogeneous_halfspace/in_data_files/Par_file | 4 ++++
homogeneous_poroelastic/in_data_files/Par_file | 6 +++++-
layered_halfspace/in_data_files/Par_file | 4 ++++
meshfem3D_examples/many_interfaces/Par_file | 4 ++++
meshfem3D_examples/simple_model/in_data_files/Par_file | 4 ++++
meshfem3D_examples/socal1D/in_data_files/Par_file | 4 ++++
tomographic_model/in_data_files/Par_file | 4 ++++
waterlayered_halfspace/in_data_files/Par_file | 4 ++++
11 files changed, 45 insertions(+), 1 deletion(-)
diff --git a/BENCHMARK_CLAERBOUT_ADJOINT/ACOUSTIC/in_data_files/Par_file b/BENCHMARK_CLAERBOUT_ADJOINT/ACOUSTIC/in_data_files/Par_file
index 4569f7e..4c5961f 100644
--- a/BENCHMARK_CLAERBOUT_ADJOINT/ACOUSTIC/in_data_files/Par_file
+++ b/BENCHMARK_CLAERBOUT_ADJOINT/ACOUSTIC/in_data_files/Par_file
@@ -77,6 +77,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .true.
diff --git a/BENCHMARK_CLAERBOUT_ADJOINT/ELASTIC/in_data_files/Par_file b/BENCHMARK_CLAERBOUT_ADJOINT/ELASTIC/in_data_files/Par_file
index 14f240b..05daef1 100644
--- a/BENCHMARK_CLAERBOUT_ADJOINT/ELASTIC/in_data_files/Par_file
+++ b/BENCHMARK_CLAERBOUT_ADJOINT/ELASTIC/in_data_files/Par_file
@@ -77,6 +77,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .true.
diff --git a/Mount_StHelens/in_data_files/Par_file b/Mount_StHelens/in_data_files/Par_file
index 03f0aed..648ddd4 100644
--- a/Mount_StHelens/in_data_files/Par_file
+++ b/Mount_StHelens/in_data_files/Par_file
@@ -77,6 +77,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .false.
diff --git a/homogeneous_halfspace/in_data_files/Par_file b/homogeneous_halfspace/in_data_files/Par_file
index 23a85c3..ae36ccf 100644
--- a/homogeneous_halfspace/in_data_files/Par_file
+++ b/homogeneous_halfspace/in_data_files/Par_file
@@ -79,6 +79,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .false.
diff --git a/homogeneous_poroelastic/in_data_files/Par_file b/homogeneous_poroelastic/in_data_files/Par_file
index 6442091..4b1ba74 100644
--- a/homogeneous_poroelastic/in_data_files/Par_file
+++ b/homogeneous_poroelastic/in_data_files/Par_file
@@ -1,4 +1,4 @@
-# simulation input parameters
+*# simulation input parameters
#
# forward or adjoint simulation
# 1 = forward, 2 = adjoint, 3 = both simultaneously
@@ -79,6 +79,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .true.
diff --git a/layered_halfspace/in_data_files/Par_file b/layered_halfspace/in_data_files/Par_file
index 15ae0a8..2f90bb2 100644
--- a/layered_halfspace/in_data_files/Par_file
+++ b/layered_halfspace/in_data_files/Par_file
@@ -78,6 +78,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .false.
diff --git a/meshfem3D_examples/many_interfaces/Par_file b/meshfem3D_examples/many_interfaces/Par_file
index 644cf66..07cfaba 100644
--- a/meshfem3D_examples/many_interfaces/Par_file
+++ b/meshfem3D_examples/many_interfaces/Par_file
@@ -78,6 +78,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .false.
diff --git a/meshfem3D_examples/simple_model/in_data_files/Par_file b/meshfem3D_examples/simple_model/in_data_files/Par_file
index 65c9914..8db6ff4 100644
--- a/meshfem3D_examples/simple_model/in_data_files/Par_file
+++ b/meshfem3D_examples/simple_model/in_data_files/Par_file
@@ -78,6 +78,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .false.
diff --git a/meshfem3D_examples/socal1D/in_data_files/Par_file b/meshfem3D_examples/socal1D/in_data_files/Par_file
index d0b9773..fb44f3a 100644
--- a/meshfem3D_examples/socal1D/in_data_files/Par_file
+++ b/meshfem3D_examples/socal1D/in_data_files/Par_file
@@ -78,6 +78,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .true.
diff --git a/tomographic_model/in_data_files/Par_file b/tomographic_model/in_data_files/Par_file
index 23f45fe..823d695 100644
--- a/tomographic_model/in_data_files/Par_file
+++ b/tomographic_model/in_data_files/Par_file
@@ -78,6 +78,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .false.
diff --git a/waterlayered_halfspace/in_data_files/Par_file b/waterlayered_halfspace/in_data_files/Par_file
index 493b1a6..2ab829c 100644
--- a/waterlayered_halfspace/in_data_files/Par_file
+++ b/waterlayered_halfspace/in_data_files/Par_file
@@ -78,6 +78,10 @@ USE_FORCE_POINT_SOURCE = .false.
# The direction vector is made unitary internally in the code and thus only its direction matters here;
# its norm is ignored and the norm of the force used is the factor force source times the source time function.
+# set to use a Ricker source time function instead of a gaussian (when using CMTSOLUTION files)
+# or a quasi-Heaviside (when using FORCESOLUTION files)
+USE_RICKER_TIME_FUNCTION = .false.
+
# print source time function
PRINT_SOURCE_TIME_FUNCTION = .false.
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