[cig-commits] [commit] master: Update README_seismic_cpml.html (db7b017)
cig_noreply at geodynamics.org
cig_noreply at geodynamics.org
Tue Feb 25 16:17:24 PST 2014
Repository : ssh://geoshell/seismic_cpml
On branch : master
Link : https://github.com/geodynamics/seismic_cpml/compare/7515e1003ff6dbacf96727c39cca65467af48b27...db7b017efaa184c4fdc84f5f67f05c17867d6302
>---------------------------------------------------------------
commit db7b017efaa184c4fdc84f5f67f05c17867d6302
Author: Dimitri Komatitsch <komatits at users.noreply.github.com>
Date: Wed Feb 26 01:17:32 2014 +0100
Update README_seismic_cpml.html
>---------------------------------------------------------------
db7b017efaa184c4fdc84f5f67f05c17867d6302
README_seismic_cpml.html | 19 +++++++------------
1 file changed, 7 insertions(+), 12 deletions(-)
diff --git a/README_seismic_cpml.html b/README_seismic_cpml.html
index 7ea21b2..da27ef2 100644
--- a/README_seismic_cpml.html
+++ b/README_seismic_cpml.html
@@ -34,7 +34,7 @@ Komatitsch and Roland Martin from University of Pau, France. </FONT>
</P>
<P STYLE="margin-bottom: 0in"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">You
can get the full source code of the programs at the official Web
-site: </FONT></FONT></FONT><A HREF="http://www.geodynamics.org/cig/software"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">http://www.geodynamics.org/cig/software</FONT></FONT></A></P>
+site: </FONT></FONT></FONT><A HREF="http://www.geodynamics.org/cig/software/"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">http://www.geodynamics.org/cig/software/</FONT></FONT></A></P>
<P><FONT SIZE=3 STYLE="font-size: 13pt">The unsplit <B>Convolutional
Perfectly Matched Layer (C-PML) for the 3D elastic wave equation</B>
was introduced and is described in detail in: </FONT>
@@ -44,8 +44,7 @@ Roland Martin,</B></FONT> <SPAN STYLE="font-variant: normal"><FONT SIZE=3 STYLE=
unsplit convolutional Perfectly Matched Layer improved at grazing
incidence for the seismic wave equation</SPAN></FONT></SPAN><FONT SIZE=3 STYLE="font-size: 13pt"><I>,
Geophysics</I></FONT><FONT SIZE=3 STYLE="font-size: 13pt">, vol.
-72(5), p SM155-SM167, doi: 10.1190/1.2757586 (2007). <A HREF="http://www.komati1/published_papers/geophysics_CPML_2007_elastic_typos_fixed.pdf">PDF
-reprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></FONT></P>
+72(5), p SM155-SM167, doi: 10.1190/1.2757586 (2007). <A HREF="http://www.komati1/published_papers/geophysics_CPML_2007_elastic_typos_fixed.pdf">Preprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></FONT></P>
<P><FONT SIZE=3 STYLE="font-size: 13pt">It was originally developed
for Maxwell's equations by Roden and Gedney (2000) (see reference
below).</FONT></P>
@@ -59,8 +58,7 @@ Journal International</SPAN></I></FONT></SPAN><SPAN STYLE="text-decoration: none
</SPAN></FONT></SPAN><SPAN STYLE="text-decoration: none"><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN LANG="fr-FR"><SPAN STYLE="font-weight: normal">vol.
179(1), p. 333-344, </SPAN></SPAN></FONT></SPAN><SPAN STYLE="font-variant: normal"><FONT COLOR="#000000"><SPAN STYLE="text-decoration: none"><FONT FACE="Times New Roman, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN LANG="fr-FR"><SPAN STYLE="font-style: normal"><SPAN STYLE="font-weight: normal">doi:
10.1111/j.1365-246X.2009.04278.x </SPAN></SPAN></SPAN></FONT></FONT></SPAN></FONT></SPAN><SPAN STYLE="text-decoration: none"><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN STYLE="font-weight: normal">(2009).</SPAN></FONT></SPAN><FONT COLOR="#000000"><SPAN STYLE="text-decoration: none">
-</SPAN></FONT><FONT COLOR="#000000"><SPAN STYLE="text-decoration: none"><FONT FACE="Times New Roman, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN LANG="fr-FR"><SPAN STYLE="font-weight: normal"><A HREF="http://komatitsch.free.fr/published_papers/GJI_CPML_2009_viscoelastic.pdf">PDF
-reprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></SPAN></SPAN></FONT></FONT></SPAN></FONT></P>
+</SPAN></FONT><FONT COLOR="#000000"><SPAN STYLE="text-decoration: none"><FONT FACE="Times New Roman, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN LANG="fr-FR"><SPAN STYLE="font-weight: normal"><A HREF="http://komatitsch.free.fr/published_papers/GJI_CPML_2009_viscoelastic.pdf">Preprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></SPAN></SPAN></FONT></FONT></SPAN></FONT></P>
<P><FONT SIZE=3 STYLE="font-size: 13pt">An extension to poroelastic
media is developed in:</FONT></P>
<P><SPAN STYLE="text-decoration: none"><FONT SIZE=3 STYLE="font-size: 13pt"><B>Roland
@@ -69,8 +67,7 @@ Martin, Dimitri Komatitsch and Abdelaâziz Ezziani</B></FONT></SPAN><FONT SIZE=3
unsplit convolutional Perfectly Matched Layer improved at grazing
incidence for seismic wave propagation in poroelastic media</SPAN></FONT></SPAN><FONT SIZE=3 STYLE="font-size: 13pt"><I>,
Geophysics</I></FONT><FONT SIZE=3 STYLE="font-size: 13pt">, vol.
-73(4), p T51-T61, doi: 10.1190/1.2939484 (2008). <A HREF="http://komatitsch.free.fr/published_papers/geophysics_CPML_2008_poroelastic_typos_fixed.pdf">PDF
-reprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></FONT></P>
+73(4), p T51-T61, doi: 10.1190/1.2939484 (2008). <A HREF="http://komatitsch.free.fr/published_papers/geophysics_CPML_2008_poroelastic_typos_fixed.pdf">Preprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></FONT></P>
<P><FONT SIZE=3 STYLE="font-size: 13pt">and a variational formulation
is developed in:</FONT></P>
<P><SPAN STYLE="text-decoration: none"><FONT SIZE=3 STYLE="font-size: 13pt"><B>Roland
@@ -82,8 +79,7 @@ A variational formulation of a stabilized unsplit convolutional
perfectly matched layer for the isotropic or anisotropic seismic wave
equation, </FONT><FONT SIZE=3 STYLE="font-size: 13pt"><I>Computer
Modeling in Engineering and Sciences</I></FONT><FONT SIZE=3 STYLE="font-size: 13pt">,
-vol. 37(3), p. 274-304 (2008). </FONT><FONT COLOR="#000000"><SPAN STYLE="text-decoration: none"><FONT FACE="Times New Roman, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN STYLE="font-weight: normal"><A HREF="http://komatitsch.free.fr/published_papers/CMES_cpml_2008.pdf">PDF
-reprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></SPAN></FONT></FONT></SPAN></FONT></P>
+vol. 37(3), p. 274-304 (2008). </FONT><FONT COLOR="#000000"><SPAN STYLE="text-decoration: none"><FONT FACE="Times New Roman, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN STYLE="font-weight: normal"><A HREF="http://komatitsch.free.fr/published_papers/CMES_cpml_2008.pdf">Preprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></SPAN></FONT></FONT></SPAN></FONT></P>
<P><FONT SIZE=3 STYLE="font-size: 13pt">An extension to higher-order
time schemes, called ADE-PML (Auxiliary Differential Equation - PML)
is developed in:</FONT></P>
@@ -94,8 +90,7 @@ matched layer for the seismic wave equation using Auxiliary
Differential Equations (ADE-PML), </SPAN></SPAN></FONT></FONT></SPAN></FONT><FONT COLOR="#000000"><SPAN STYLE="text-decoration: none"><FONT FACE="Times New Roman, serif"><FONT SIZE=4><SPAN LANG="fr-FR"><I><SPAN STYLE="font-weight: normal">Computer
Modeling in Engineering and Sciences</SPAN></I></SPAN></FONT></FONT></SPAN></FONT><FONT COLOR="#000000"><SPAN STYLE="text-decoration: none"><FONT FACE="Times New Roman, serif"><FONT SIZE=4><SPAN LANG="fr-FR"><SPAN STYLE="font-weight: normal">,
vol. 56(1), p. 17-42 (2010).</SPAN></SPAN></FONT></FONT></SPAN></FONT>
-<FONT SIZE=3 STYLE="font-size: 13pt"><A HREF="http://komatitsch.free.fr/published_papers/CMES_ADE_PML_2010.pdf">PDF
-reprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></FONT></P>
+<FONT SIZE=3 STYLE="font-size: 13pt"><A HREF="http://komatitsch.free.fr/published_papers/CMES_ADE_PML_2010.pdf">Preprint</A> <A HREF="http://komatitsch.free.fr/bibtex_komatitsch.bib">BibTeX</A></FONT></P>
<P><FONT SIZE=3 STYLE="font-size: 13pt">Note that in the case of an
anisotropic medium the modification made is not strictly speaking
perfectly matched any more, i.e., not a PML, but rather </FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">a
@@ -161,7 +156,7 @@ is:</FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, seri
Arbitrary Media},<BR>journal = {Microwave and Optical Technology
Letters},<BR>year = {2000},<BR>volume = {27},<BR>number = {5},<BR>pages
= {334-339},<BR>doi =
-{10.1002/1098-2760(20001205)27:5<334::AID-MOP14>3.0.CO;2-A}}<BR></FONT></FONT><A HREF="http://www.geodynamics.org/cig/software"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=1 STYLE="font-size: 6pt"><B><BR><BR></B></FONT></FONT></FONT></A><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN STYLE="font-weight: normal">The
+{10.1002/1098-2760(20001205)27:5<334::AID-MOP14>3.0.CO;2-A}}<BR></FONT></FONT><A HREF="http://www.geodynamics.org/cig/software/"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=1 STYLE="font-size: 6pt"><B><BR><BR></B></FONT></FONT></FONT></A><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN STYLE="font-weight: normal">The
package is composed of the following </SPAN></FONT><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN STYLE="font-weight: normal">eleven
</SPAN></FONT><FONT SIZE=3 STYLE="font-size: 13pt"><SPAN STYLE="font-weight: normal">programs:</SPAN></FONT></P>
<P STYLE="margin-bottom: 0in"><BR>
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