[cig-commits] r15758 - in doc/geodynamics.org/benchmarks/trunk: . cs mc short/rs/results short/rs-nog/geofest-input short/rs-nog/pylith-0.8-input short/rs-nog/results short/strikeslip/geofest-input short/strikeslip/pylith-0.8-input short/strikeslip/results short/utilities
luis at geodynamics.org
luis at geodynamics.org
Mon Oct 5 15:40:39 PDT 2009
Author: luis
Date: 2009-10-05 15:40:35 -0700 (Mon, 05 Oct 2009)
New Revision: 15758
Removed:
doc/geodynamics.org/benchmarks/trunk/cs/index.html
doc/geodynamics.org/benchmarks/trunk/index.html
doc/geodynamics.org/benchmarks/trunk/mc/notes-on-mantle-convection-benchmarks.html
doc/geodynamics.org/benchmarks/trunk/short/rs-nog/geofest-input/index.html
doc/geodynamics.org/benchmarks/trunk/short/rs-nog/pylith-0.8-input/index.html
doc/geodynamics.org/benchmarks/trunk/short/rs-nog/results/index.html
doc/geodynamics.org/benchmarks/trunk/short/rs/results/index.html
doc/geodynamics.org/benchmarks/trunk/short/strikeslip/geofest-input/index.html
doc/geodynamics.org/benchmarks/trunk/short/strikeslip/pylith-0.8-input/index.html
doc/geodynamics.org/benchmarks/trunk/short/strikeslip/results/index.html
doc/geodynamics.org/benchmarks/trunk/short/utilities/CUBITex.html
doc/geodynamics.org/benchmarks/trunk/short/utilities/index.html
Log:
Don't generate these html files yet.
For now, we only generate the html files listed in "upload.txt".
Deleted: doc/geodynamics.org/benchmarks/trunk/cs/index.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/cs/index.html 2009-10-05 22:40:24 UTC (rev 15757)
+++ doc/geodynamics.org/benchmarks/trunk/cs/index.html 2009-10-05 22:40:35 UTC (rev 15758)
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===================================================================
--- doc/geodynamics.org/benchmarks/trunk/index.html 2009-10-05 22:40:24 UTC (rev 15757)
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-<li><a class="reference external" href="http://geodynamics.org/cig/software/benchmarks/short/">Short-Term Crustal Dynamics</a></li>
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===================================================================
--- doc/geodynamics.org/benchmarks/trunk/mc/notes-on-mantle-convection-benchmarks.html 2009-10-05 22:40:24 UTC (rev 15757)
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-<div class="document" id="notes-on-mantle-convection-benchmarks">
-<h1 class="title">Notes On Mantle Convection Benchmarks</h1>
-
-<p>(1) Ra = 3x10**6 (I think this is high enough to give some real time
-dependence without pushing available resolution very much).</p>
-<p>(2) Constaint properties (thermal expansivity, thermal diffusivity,
-density, gravity, viscosity, internal heat generation) to keep things
-very simple.</p>
-<ol class="arabic simple" start="3">
-<li>Free slip upper and lower boundaries.</li>
-<li>Radius ratio = 0.546 (cmb/surface radius)</li>
-<li>purely internally heated</li>
-<li>insulating at cmb, constant temperature at surface</li>
-</ol>
-<p>(7) model resolution: 65 nodes (64 layers) radially, with some packing of
-nodes near the top and bottom boundaries. (We'll send you the actual
-radii we use, assuming you can vary them at will.)</p>
-<p>(8) initial diagnostics: (basically, these are just to get started and
-see if we're in the same universe)</p>
-<ul class="simple">
-<li>(a) Nu vs. time (this should square with the internal heating in a
-time-average sense)</li>
-<li>(b) Radial temperature profile vs. time - this is effectively a
-measure of the efficiency of heat transfer, or equivalent of Nu for
-bottom heated cases.</li>
-<li>(c) Spherical harmonic expansion of temperature field at all radial
-levels at beginning and ending time (see below).</li>
-<li><ol class="first loweralpha" start="4">
-<li>peak velocity and peak temperature in each radial layer vs. time</li>
-</ol>
-</li>
-<li>(e) for now, let's ignore dynamic topography, since it's derived from
-primitive results</li>
-</ul>
-<p>(9) Initial conditions and run time: This is a bit thorny, so here's a
-proposal. We can run TERRA to equilibrium under the specified model
-conditions. Equilibrium is where Nu has settled down to fluctuations
-about a steady mean value. At some point, call it time = 0.0, we'll stop
-the code and output the full temperature field in the form of a spherical
-harmonic expansion up to degree 128, which corresponds to the highest
-model resolution. We can then restart both TERRA and CitcomS using this
-spherical harmonic expansion (NOT the full temperature field at each
-node, since this would prejudice things with regard to the particular
-horizontal discretization.) Then both codes can run for a defined amount
-of model time, keeping track of Nu, peak T, and peak V as a function of
-time as indicated above. At the end of this time, or at several times
-along the way, we can output spherical harmonic representations of T at
-each layer for comparison.</p>
-<p>I added the following comments:</p>
-<p>(1) We use some analytic expressions for initial conditions (e.g., some
-radial profile superimposed with a small perturbation of a given harmonic
-function). In this way, others, if they want to benchmark their codes, do
-not need to get the Terra output. Also in case some summary report comes
-out of this effort, we can simply write down the initial conditions.</p>
-<p>(2) We aim to reproduce four benchmark cases in steady of just one. The
-four cases at the moment in my mind can be: three constant property cases
-with purely basal heating at Ra=1e5 (case 1), and Ra=1e6 (case 2), and
-purely internal heating at Ra=1e6 (case 3), and one temperature dependent
-viscosity and purely basal heating at Ra=1e6 (case 4).</p>
-<p>Case 1 will likely reach to a steady state, which is always a good thing
-for a benchmark. Cases 2 and 3 are almost identical to what you have
-suggested recently, and they are most likely time-dependent. The 1e6 Ra
-is smaller than what you suggested today but is consistent with your
-earlier suggestion. With Ra=1e6, we may not need grid refinement, which
-is also good for benchmark purposes (again, others can do it later).
-Case 4 is obviously of interest too.</p>
-</div>
-</body>
-</html>
Deleted: doc/geodynamics.org/benchmarks/trunk/short/rs/results/index.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/short/rs/results/index.html 2009-10-05 22:40:24 UTC (rev 15757)
+++ doc/geodynamics.org/benchmarks/trunk/short/rs/results/index.html 2009-10-05 22:40:35 UTC (rev 15758)
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-<dt>Plone Metadata</dt>
-<dd><p class="first">results</p>
-<p>Results</p>
-<p class="last">Results from benchmark runs. Place tarballs containing the requested results
-in this folder and describe the run in the <cite>description</cite> field.</p>
-</dd>
-<dt>URL</dt>
-<dd><a class="reference external" href="http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/benchmark-rs/results">http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/benchmark-rs/results</a></dd>
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Deleted: doc/geodynamics.org/benchmarks/trunk/short/rs-nog/geofest-input/index.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/short/rs-nog/geofest-input/index.html 2009-10-05 22:40:24 UTC (rev 15757)
+++ doc/geodynamics.org/benchmarks/trunk/short/rs-nog/geofest-input/index.html 2009-10-05 22:40:35 UTC (rev 15758)
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-<li><dl class="first docutils">
-<dt>bmrsnog_tet4_1000m.gft.gz (2006-08-31)</dt>
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-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>bmrsnog_tet4_0500m.gft.gz (2006-08-31)</dt>
-<dd><p class="first last">Gzipped GeoFEST input file for benchmark using linear tetrahedral elements
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-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>reverse slip (no grav), refined grid 01, no smoothing (GeoFEST 4.5)</dt>
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Deleted: doc/geodynamics.org/benchmarks/trunk/short/rs-nog/pylith-0.8-input/index.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/short/rs-nog/pylith-0.8-input/index.html 2009-10-05 22:40:24 UTC (rev 15757)
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-<blockquote>
-<ul>
-<li><dl class="first docutils">
-<dt>bmrsnog_hex_1000m.tgz (2006-07-20)</dt>
-<dd><p class="first last">Tarball containing PyLith-0.8 input files for benchmark using linear hexahedral
-elements with a 1000m nominal node spacing.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>bmrsnog_tet4_1000m.tgz (2006-07-20)</dt>
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-elements with a 1000m nominal node spacing.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>bmrsnog_tet4_0500m.tgz (2006-07-20)</dt>
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-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>bmrsnog_tet4_0250m.tgz (2006-07-20)</dt>
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-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>reverse slip (no grav), refined grid 01, no smoothing (2006-09-06)</dt>
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-see <a class="reference external" href="http://meshing.lanl.gov/proj/crustal_dyn_reverse_fault_bm/catalog.html">http://meshing.lanl.gov/proj/crustal_dyn_reverse_fault_bm/catalog.html</a></p>
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-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>reverse slip (no grav), refined grid 02, no smoothing (2006-09-06)</dt>
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-</dl>
-</li>
-</ul>
-</blockquote>
-</blockquote>
-<dl class="docutils">
-<dt>URL</dt>
-<dd><a class="reference external" href="http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/benchmark-rs-nog/pylith-0.8-input">http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/benchmark-rs-nog/pylith-0.8-input</a></dd>
-</dl>
-</div>
-</body>
-</html>
Deleted: doc/geodynamics.org/benchmarks/trunk/short/rs-nog/results/index.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/short/rs-nog/results/index.html 2009-10-05 22:40:24 UTC (rev 15757)
+++ doc/geodynamics.org/benchmarks/trunk/short/rs-nog/results/index.html 2009-10-05 22:40:35 UTC (rev 15758)
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-<p>Results</p>
-<blockquote>
-<p>Results from benchmark runs. Place tarballs containing the requested results
-in this folder and describe the run in the description field.</p>
-<blockquote>
-<ul>
-<li><dl class="first docutils">
-<dt>GeoFEST reverse fault results - 1 km (2006-08-17)</dt>
-<dd><p class="first last">Tarball contains input and output files as well as text file
-containing run-time information</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>GeoFEST reverse fault results - 500 m (2006-08-17)</dt>
-<dd><p class="first last">Tarball contains input and output files as well as text file
-containing run-time information</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>Geofest reverse slip var_res_mesh_01_soln (2006-09-05)</dt>
-<dd><p class="first last">fixed the BCs, Geofest 4.5, dt=0.1 constant</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>PyLith, 1 proc, linear hex, 1 km resolution, dt=0.1yr (2006-08-29)</dt>
-<dd><p class="first last">PyLith results run on 1 processor of a Power Mac G5.
-Linear hexahedral mesh at 1 km resolution.
-Constant time step size of 0.1 years.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>PyLith, 1 proc, linear tet, 1 km resolution, dt=0.1yr (2006-08-29)</dt>
-<dd><p class="first last">PyLith results run on 1 processor of a Power Mac G5.
-Linear tetrahedral mesh at 1 km resolution.
-Constant time step size of 0.1 years.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>PyLith, 1 proc, linear tet, 500 m resolution, dt=0.1yr (2006-08-29)</dt>
-<dd><p class="first last">PyLith results run on 1 processor of a Power Mac G5.
-Linear tetrahedral mesh at 500 m resolution.
-Constant time step size of 0.1 years.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>PyLith, 1 proc, linear tet, 250 m resolution, dt=0.1yr (2006-08-29)</dt>
-<dd><p class="first last">PyLith results run on 1 processor of a Power Mac G5.
-Linear tetrahedral mesh at 250 m resolution.
-Constant time step size of 0.1 years.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>tet_var_res_01_pylith_soln.tgz (2006-09-04)</dt>
-<dd><p class="first last">PyLith-0.8 results for Carl Gable's variable resolution (no smoothing)
-mesh 01 for the reverse slip benchmark - constant dt=0.1yr</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>Femlab 2 km resolution, elastic (2006-10-16)</dt>
-<dd><p class="first last">This model has 19544 quadratic tetrahedral elements and is twice the
-size in y of the model description, since there is no symmetric boundary.
-This yields a resolution close to 2 km. The model and solver require
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-<dd><a class="reference external" href="http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/benchmark-rs-nog/results">http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/benchmark-rs-nog/results</a></dd>
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Deleted: doc/geodynamics.org/benchmarks/trunk/short/strikeslip/geofest-input/index.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/short/strikeslip/geofest-input/index.html 2009-10-05 22:40:24 UTC (rev 15757)
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-</dl>
-</div>
-</body>
-</html>
Deleted: doc/geodynamics.org/benchmarks/trunk/short/strikeslip/pylith-0.8-input/index.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/short/strikeslip/pylith-0.8-input/index.html 2009-10-05 22:40:24 UTC (rev 15757)
+++ doc/geodynamics.org/benchmarks/trunk/short/strikeslip/pylith-0.8-input/index.html 2009-10-05 22:40:35 UTC (rev 15758)
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Deleted: doc/geodynamics.org/benchmarks/trunk/short/strikeslip/results/index.html
===================================================================
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-<body>
-<div class="document">
-
-
-<p>Results</p>
-<blockquote>
-<p>Results from benchmark runs. Place tarballs containing the requested results
-in this folder, and describe the run in the description field.</p>
-<blockquote>
-<ul>
-<li><dl class="first docutils">
-<dt>PyLith, 1 proc, linear tet, 1km resolution, dt=0.1yr (2006-08-29)</dt>
-<dd><p class="first last">PyLith results run on 1 processor of a Power Mac G5.
-Linear tetrahedral mesh at 1km resolution.
-Constant time step size of 0.1 year.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>PyLith, 1 proc, linear hex, 1km resolution, dt=0.1yr (2006-08-29)</dt>
-<dd><p class="first last">PyLith results on 1 processor of a Power Mac G5.
-Linear hexahedral mesh at 1km resolution.
-Constant time step size of 0.1 year.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>PyLith, 1 proc, linear tet, 500m resolution, dt=0.1yr (2006-08-29)</dt>
-<dd><p class="first last">PyLith results run on 1 processor of a Power Mac G5.
-Linear tetrahedral mesh at 500m resolution.
-Constant time step size of 0.1 year.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>PyLith Revised Results, 500m, New BC and Split Node Input (2007-01-30)</dt>
-<dd><p class="first last">New solution using revised BC and split node inputs. The revised BC
-take care of the problems of defining BC on the fault plane (or in
-some cases the projected fault plane). The new split node inputs
-no longer assume a bilinear slip distribution in the region where
-the fault tapers overlap, and now assumes a taper consistent with
-what is used for the analytical solution.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>PyLith Revised Results, 500m, Altered BC for Viscoelastic Solution (2007-02-06)</dt>
-<dd><p class="first last">New version where BC have been altered from those of previous version
-to make viscoelastic results consistent with those from GeoFEST.
-The revised BC do not pin y-component on the y=0 plane, and no BC
-are applied along the intersection of the fault plane (or its projection)
-along y=0 and z=-24.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>PyLith, 1 proc, linear tet, 250m resolution, dt=0.1yr (2006-09-07)</dt>
-<dd><p class="first last">PyLith results run on 1 processor of an Opteron 2.4GHz Linux machine.
-Linear tetrahedral mesh at 250m resolution.
-Constant time step size of 0.1 year.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>GeoFEST / PYRAMID 1km (2006-09-06)</dt>
-<dd><p class="first last">Parallel results using 64 processors of Intel/Linux Cluster
-with GeoFEST-4.5 and Pyramid-2.1.3</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>GeoFEST / PYRAMID 500m (2006-09-06)</dt>
-<dd><p class="first last">Parallel results using 64 processors of Intel/Linux Cluster
-with GeoFEST-4.5 and Pyramid-2.1.3</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>GeoFEST / PYRAMID 250m (2006-09-06)</dt>
-<dd><p class="first last">Parallel results using 128 processors of Intel/Linux Cluster
-with GeoFEST-4.5 and Pyramid-2.1.3</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>GeoFEST linear tet 1km resolution dt=0.1yr (updated) (2006-09-21)</dt>
-<dd><p class="first last">The taper error has been fixed.</p>
-</dd>
-</dl>
-</li>
-<li><p class="first">GeoFEST Linear-Tet 500m Re-Run (2006-11-29)</p>
-</li>
-<li><p class="first">GeoFEST Linear-Tet 250m Re-Run (2006-11-29)</p>
-</li>
-<li><dl class="first docutils">
-<dt>Femlab 1km resolution, t = 0 years (2006-10-17)</dt>
-<dd><p class="first last">This model has ~162,000 linear tetrahedral elements and is twice the
-size in y of the model description, since there is no symmetric boundary.
-This yields a resolution close to 1km. The model and solver require
-almost 800MB and is solved in about 3 minutes on a 1.8 GHz AMD Opteron.
-An iterative solver was used, which uses the Incomplete LU preconditioner
-with a drop tolerance of 0.01. Decreasing this value has very little
-effect on the error but takes longer to solve.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>Femlab 1km resolution, t = 1 year (2006-10-17)</dt>
-<dd><p class="first last">Viscoelastic problem requires ~3.5GB and takes about 4.5 hours to run.
-Drop tolerance is 0.01.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>Femlab 1km resolution, t = 5 years (2006-10-17)</dt>
-<dd><p class="first last">Viscoelastic problem requires ~3.5GB and takes about 4.5 hours to run.
-Drop tolerance is 0.01.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>Femlab 1km resolution, t = 10 years (2006-10-17)</dt>
-<dd><p class="first last">Viscoelastic problem requires ~3.5GB and takes about 4.5 hours to run.
-Drop tolerance is 0.01.</p>
-</dd>
-</dl>
-</li>
-</ul>
-</blockquote>
-</blockquote>
-<dl class="docutils">
-<dt>URL</dt>
-<dd><a class="reference external" href="http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/benchmark-strikeslip/results">http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/benchmark-strikeslip/results</a></dd>
-</dl>
-</div>
-</body>
-</html>
Deleted: doc/geodynamics.org/benchmarks/trunk/short/utilities/CUBITex.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/short/utilities/CUBITex.html 2009-10-05 22:40:24 UTC (rev 15757)
+++ doc/geodynamics.org/benchmarks/trunk/short/utilities/CUBITex.html 2009-10-05 22:40:35 UTC (rev 15758)
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-<p>Example Journal Files for CUBIT</p>
-<blockquote>
-<p>From the 2009 NMCDEF meeting in Golden, CO</p>
-<blockquote>
-<ul>
-<li><dl class="first docutils">
-<dt>Meshing example (2009-06-23)</dt>
-<dd><p class="first last">Very short example of meshing a pyramid and displaying mesh</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>Geometry test (2009-06-23)</dt>
-<dd><p class="first last">Example of building geometrical shapes with merging, subtracting, moving, etc.</p>
-</dd>
-</dl>
-</li>
-<li><dl class="first docutils">
-<dt>Fault example (2009-06-23)</dt>
-<dd><p class="first last">Example of building and meshing (coarsely) a region around a dipping fault patch.</p>
-</dd>
-</dl>
-</li>
-</ul>
-</blockquote>
-</blockquote>
-<dl class="docutils">
-<dt>URL</dt>
-<dd><a class="reference external" href="http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/utilities/CUBITex">http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/utilities/CUBITex</a></dd>
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-</html>
Deleted: doc/geodynamics.org/benchmarks/trunk/short/utilities/index.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/short/utilities/index.html 2009-10-05 22:40:24 UTC (rev 15757)
+++ doc/geodynamics.org/benchmarks/trunk/short/utilities/index.html 2009-10-05 22:40:35 UTC (rev 15758)
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- border: medium outset ;
- padding: 1em }
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-div.admonition p.admonition-title, div.hint p.admonition-title,
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- font-weight: bold ;
- font-family: sans-serif }
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-div.attention p.admonition-title, div.caution p.admonition-title,
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- color: red ;
- font-weight: bold ;
- font-family: sans-serif }
-
-/* Uncomment (and remove this text!) to get reduced vertical space in
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-div.compound .compound-last, div.compound .compound-middle {
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- text-align: center ;
- font-style: italic }
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- font-weight: bold ;
- font-style: normal }
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-div.figure {
- margin-left: 2em ;
- margin-right: 2em }
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- font-size: smaller }
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-div.line-block {
- display: block ;
- margin-top: 1em ;
- margin-bottom: 1em }
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- margin-left: 1.5em }
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-div.sidebar {
- margin: 0 0 0.5em 1em ;
- border: medium outset ;
- padding: 1em ;
- background-color: #ffffee ;
- width: 40% ;
- float: right ;
- clear: right }
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- font-family: sans-serif ;
- font-size: medium }
-
-div.system-messages {
- margin: 5em }
-
-div.system-messages h1 {
- color: red }
-
-div.system-message {
- border: medium outset ;
- padding: 1em }
-
-div.system-message p.system-message-title {
- color: red ;
- font-weight: bold }
-
-div.topic {
- margin: 2em }
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-h1.section-subtitle, h2.section-subtitle, h3.section-subtitle,
-h4.section-subtitle, h5.section-subtitle, h6.section-subtitle {
- margin-top: 0.4em }
-
-h1.title {
- text-align: center }
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- text-align: center }
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-hr.docutils {
- width: 75% }
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-img.align-left {
- clear: left }
-
-img.align-right {
- clear: right }
-
-ol.simple, ul.simple {
- margin-bottom: 1em }
-
-ol.arabic {
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-ol.loweralpha {
- list-style: lower-alpha }
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- font-size: larger ;
- color: maroon ;
- text-align: center }
-
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- font-family: sans-serif ;
- font-weight: bold ;
- font-size: larger }
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-p.sidebar-subtitle {
- font-family: sans-serif ;
- font-weight: bold }
-
-p.topic-title {
- font-weight: bold }
-
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- margin-bottom: 0 ;
- margin-top: 0 ;
- font-family: serif ;
- font-size: 100% }
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-span.interpreted {
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-span.option {
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- color: red }
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- /* font-size relative to parent (h1..h6 element) */
- font-size: 80% }
-
-table.citation {
- border-left: solid 1px gray;
- margin-left: 1px }
-
-table.docinfo {
- margin: 2em 4em }
-
-table.docutils {
- margin-top: 0.5em ;
- margin-bottom: 0.5em }
-
-table.footnote {
- border-left: solid 1px black;
- margin-left: 1px }
-
-table.docutils td, table.docutils th,
-table.docinfo td, table.docinfo th {
- padding-left: 0.5em ;
- padding-right: 0.5em ;
- vertical-align: top }
-
-table.docutils th.field-name, table.docinfo th.docinfo-name {
- font-weight: bold ;
- text-align: left ;
- white-space: nowrap ;
- padding-left: 0 }
-
-h1 tt.docutils, h2 tt.docutils, h3 tt.docutils,
-h4 tt.docutils, h5 tt.docutils, h6 tt.docutils {
- font-size: 100% }
-
-ul.auto-toc {
- list-style-type: none }
-
-</style>
-</head>
-<body>
-<div class="document">
-
-
-<dl class="docutils">
-<dt>URL</dt>
-<dd><a class="reference external" href="http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/utilities">http://geodynamics.org/cig/workinggroups/short/workarea/benchmarks/utilities</a></dd>
-</dl>
-</div>
-</body>
-</html>
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