[cig-commits] r15924 - in seismo/3D/CPML: tags/v1.1.0 trunk

dkomati1 at geodynamics.org dkomati1 at geodynamics.org
Tue Nov 3 13:26:13 PST 2009 

Author: dkomati1
Date: 2009-11-03 13:26:13 -0800 (Tue, 03 Nov 2009)
New Revision: 15924

Modified:
   seismo/3D/CPML/tags/v1.1.0/README_seismic_cpml.html
   seismo/3D/CPML/trunk/README_seismic_cpml.html
Log:
added the download map to the HTML manual


Modified: seismo/3D/CPML/tags/v1.1.0/README_seismic_cpml.html
===================================================================
--- seismo/3D/CPML/tags/v1.1.0/README_seismic_cpml.html	2009-11-03 21:22:14 UTC (rev 15923)
+++ seismo/3D/CPML/tags/v1.1.0/README_seismic_cpml.html	2009-11-03 21:26:13 UTC (rev 15924)
@@ -3,6 +3,10 @@
 <HEAD>
 	<META HTTP-EQUIV="CONTENT-TYPE" CONTENT="text/html; charset=utf-8">
 	<TITLE>The SEISMIC_CPML software package</TITLE>
+	<META NAME="GENERATOR" CONTENT="OpenOffice.org 3.0  (Linux)">
+	<META NAME="CREATED" CONTENT="0;0">
+	<META NAME="CHANGEDBY" CONTENT="Dimitri Komatitsch">
+	<META NAME="CHANGED" CONTENT="20091103;22190500">
 	<STYLE TYPE="text/css">
 	<!--
 		P { color: #000000; font-family: "Times New Roman"; font-size: 12pt }
@@ -16,6 +20,9 @@
 Komatitsch</A></P>
 <P ALIGN=CENTER><A NAME="_x0000_i1025"></A><IMG SRC="http://www.univ-pau.fr/~dkomati1/seismic_cpml.gif" NAME="graphics1" ALIGN=BOTTOM WIDTH=158 HEIGHT=30 BORDER=0></P>
 <P>&nbsp;</P>
+<P ALIGN=CENTER><A NAME="download_map"></A><IMG SRC="http://www.geodynamics.org/~buildbot/maps/Seismic_CPML.gif" NAME="download_map2" ALIGN=BOTTOM BORDER=0></P>
+<P><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><center><u><b>Current SEISMIC_CPML download map since its first release</b></u></center></FONT></FONT></FONT></P>
+<P>&nbsp;</P>
 <P><FONT COLOR="#ff0000"><FONT SIZE=3 STYLE="font-size: 13pt">SEISMIC_CPML
 is a set of eight open-source Fortran90 programs</FONT></FONT> <FONT SIZE=3 STYLE="font-size: 13pt">to
 solve the two-dimensional or three-dimensional isotropic or
@@ -24,11 +31,10 @@
 (C-PML) conditions, developed by Dimitri Komatitsch and Roland Martin
 from University of Pau, France. </FONT>
 </P>
-<P STYLE="margin-bottom: 0in"><FONT SIZE=3 STYLE="font-size: 13pt"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif">You
-can get the full source code of the programs at the official
-Web site:
-</FONT></FONT><A HREF="http://www.geodynamics.org/cig/software/packages/seismo/seismic_cpml"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><B>http://www.geodynamics.org/cig/software/packages/seismo/seismic_cpml</B></FONT></FONT></A><A HREF="http://www.geodynamics.org/cig/software/packages/seismo/seismic_cpml"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=1 STYLE="font-size: 6pt"><B><BR></B></FONT></FONT></FONT></A></FONT><BR>
-</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/packages/seismo/seismic_cpml"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><B>http://www.geodynamics.org/cig/software/packages/seismo/seismic_cpml</B></FONT></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>
@@ -81,8 +87,7 @@
 <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
-“Modified PML / M-PML” based on Meza-Fajardo
- and  Papageorgiou,
+“Modified PML / M-PML” based on Meza-Fajardo and Papageorgiou,
 </FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><I>Bulletin
 of the Seismological Society of America</I></FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">,
 vol. 98(4), p. 1811-1836 (2008). H</FONT></FONT></FONT><FONT SIZE=3 STYLE="font-size: 13pt">owever,
@@ -142,8 +147,7 @@
 <P><FONT COLOR="#ff0000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><B>seismic_CPML_2D_anisotropic.f90</B></FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">:
 2D C-PML program for an anisotropic medium using a second-order
 finite-difference spatial operator. More precisely we implement a
-“Modified PML / M-PML” based on Meza-Fajardo
- and  Papageorgiou,
+“Modified PML / M-PML” based on Meza-Fajardo and Papageorgiou,
 </FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><I>Bulletin
 of the Seismological Society of America</I></FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">,
 vol. 98(4), p. 1811-1836 (2008). Strictly speaking the layers are not

Modified: seismo/3D/CPML/trunk/README_seismic_cpml.html
===================================================================
--- seismo/3D/CPML/trunk/README_seismic_cpml.html	2009-11-03 21:22:14 UTC (rev 15923)
+++ seismo/3D/CPML/trunk/README_seismic_cpml.html	2009-11-03 21:26:13 UTC (rev 15924)
@@ -3,6 +3,10 @@
 <HEAD>
 	<META HTTP-EQUIV="CONTENT-TYPE" CONTENT="text/html; charset=utf-8">
 	<TITLE>The SEISMIC_CPML software package</TITLE>
+	<META NAME="GENERATOR" CONTENT="OpenOffice.org 3.0  (Linux)">
+	<META NAME="CREATED" CONTENT="0;0">
+	<META NAME="CHANGEDBY" CONTENT="Dimitri Komatitsch">
+	<META NAME="CHANGED" CONTENT="20091103;22190500">
 	<STYLE TYPE="text/css">
 	<!--
 		P { color: #000000; font-family: "Times New Roman"; font-size: 12pt }
@@ -16,6 +20,9 @@
 Komatitsch</A></P>
 <P ALIGN=CENTER><A NAME="_x0000_i1025"></A><IMG SRC="http://www.univ-pau.fr/~dkomati1/seismic_cpml.gif" NAME="graphics1" ALIGN=BOTTOM WIDTH=158 HEIGHT=30 BORDER=0></P>
 <P>&nbsp;</P>
+<P ALIGN=CENTER><A NAME="download_map"></A><IMG SRC="http://www.geodynamics.org/~buildbot/maps/Seismic_CPML.gif" NAME="download_map2" ALIGN=BOTTOM BORDER=0></P>
+<P><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><center><u><b>Current SEISMIC_CPML download map since its first release</b></u></center></FONT></FONT></FONT></P>
+<P>&nbsp;</P>
 <P><FONT COLOR="#ff0000"><FONT SIZE=3 STYLE="font-size: 13pt">SEISMIC_CPML
 is a set of eight open-source Fortran90 programs</FONT></FONT> <FONT SIZE=3 STYLE="font-size: 13pt">to
 solve the two-dimensional or three-dimensional isotropic or
@@ -24,11 +31,10 @@
 (C-PML) conditions, developed by Dimitri Komatitsch and Roland Martin
 from University of Pau, France. </FONT>
 </P>
-<P STYLE="margin-bottom: 0in"><FONT SIZE=3 STYLE="font-size: 13pt"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif">You
-can get the full source code of the programs at the official
-Web site:
-</FONT></FONT><A HREF="http://www.geodynamics.org/cig/software/packages/seismo/seismic_cpml"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><B>http://www.geodynamics.org/cig/software/packages/seismo/seismic_cpml</B></FONT></FONT></A><A HREF="http://www.geodynamics.org/cig/software/packages/seismo/seismic_cpml"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=1 STYLE="font-size: 6pt"><B><BR></B></FONT></FONT></FONT></A></FONT><BR>
-</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/packages/seismo/seismic_cpml"><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><B>http://www.geodynamics.org/cig/software/packages/seismo/seismic_cpml</B></FONT></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>
@@ -81,8 +87,7 @@
 <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
-“Modified PML / M-PML” based on Meza-Fajardo
- and  Papageorgiou,
+“Modified PML / M-PML” based on Meza-Fajardo and Papageorgiou,
 </FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><I>Bulletin
 of the Seismological Society of America</I></FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">,
 vol. 98(4), p. 1811-1836 (2008). H</FONT></FONT></FONT><FONT SIZE=3 STYLE="font-size: 13pt">owever,
@@ -142,8 +147,7 @@
 <P><FONT COLOR="#ff0000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><B>seismic_CPML_2D_anisotropic.f90</B></FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">:
 2D C-PML program for an anisotropic medium using a second-order
 finite-difference spatial operator. More precisely we implement a
-“Modified PML / M-PML” based on Meza-Fajardo
- and  Papageorgiou,
+“Modified PML / M-PML” based on Meza-Fajardo and Papageorgiou,
 </FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt"><I>Bulletin
 of the Seismological Society of America</I></FONT></FONT></FONT><FONT COLOR="#000000"><FONT FACE="Liberation Serif, serif"><FONT SIZE=3 STYLE="font-size: 13pt">,
 vol. 98(4), p. 1811-1836 (2008). Strictly speaking the layers are not

More information about the CIG-COMMITS mailing list