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<!DOCTYPE html>
<html lang="en">
<head>
<meta charset="utf-8">
<meta name="viewport" content="width=device-width, initial-scale=1.0, user-scalable=no">
<meta name="description" content="Sediment Transport Geological Scale">
<meta name="author" content="Tristan Salles">
<title>SgFm - Sediment Transport @ Geological Scale</title>
<!-- Bootstrap Core CSS -->
<link href="css/bootstrap.min.css" rel="stylesheet" type="text/css">
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<span style="font-family:Montserrat; font-size:17px; font-weight:normal;">GIS Input Generation</a></span></li>
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<span style="font-family:Montserrat; font-size:17px; font-weight:normal;">Visualisation Tips</a></span></li>
<li><a href="http://tristan-salles.github.io/SGFM-website/cookbook.html">
<span style="font-family:Montserrat; font-size:17px; font-weight:normal;">Cookbook Examples</a></span></li>
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<ul class="nav navbar-nav navbar-right">
<li class="hidden">
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</li>
<li class="page-scroll">
<a href="#delta">DELTA</a>
</li>
<li class="page-scroll">
<a href="#ridge">RIDGE</a>
</li>
<li class="page-scroll">
<a href="#s2s">S2S</a>
</li>
<li class="page-scroll">
<a href="#rift">RIFT</a>
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<header>
<div class="container">
<div class="row">
<div class="col-lg-12">
<img class="img-responsive" src="img/cookbook.png" alt="">
<div class="intro-text">
<span class="name">Cookbook</span>
<span class="skills">Lecode Recipes</span>
</div>
</div>
</div>
</div>
</header>
<section id="overview">
<br><br>
<div class="container">
<div class="row">
<div class="col-lg-12 text-left">
<p> The following is the list of hands-on examples supported by the <a href="https://github.com/lecode-model" target="_blank">SGFM Team</a>.
These applications are provided with Lecode code base and cover its main capabilities.
<br>
These will help you to familiarise with the code. There are other applications which will be publicly released in the future.
</br>
To run an example you will need to open a Terminal, move to the chosen folder and use the following command:
<pre><code>$ mpirun -np X /path-to-lecode-folder/bin/lecode inputfile.xml
</code></pre><p>
Where <code>X</code> is the number of processors you want to use, <code>path-to-lecode-folder</code> is quite self explanatory and <code>inputfile.xml</code> is the XmL input file
located in the example folder.</p>
</div>
<div class="col-lg-12 text-center">
<hr class="star-primary">
</div>
</section>
<section id="delta">
<div class="container">
<div class="row">
<div class="col-lg-12">
<h2>Delta application</h2>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-left">
<p>
The model has been applied to understand the relative importance of sediment supply over fault-controlled
accommodation space in controlling the along-strike variability in shelf-margin and upper slope architecture of the Bonaparte Basin (NW Australia).
<br>
<strong>Lecode</strong> allows the quantification of the range of:
<i>(1)</i> sedimentation rates;
<i>(2)</i> global shelf-margin subsidence; and
<i> (3)</i> local fault-induced subsidence values
necessary to reconstruct the 3D architecture of the shelf-margin delta and the Bonaparte Basin.
</p>
</div>
</div>
<div class="row">
<div class="col-xs-8 col-xs-offset-2"><br>
<img src="figures/delta1.png" class="img-responsive img-centered" alt=""><br>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-left">
<p>
Here, the proposed example simulates the first part of the Bonaparte Delta progradation.
To get more details on the results of <strong>Lecode</strong> Bonaparte Delta simulation see
<a href="http://www.searchanddiscovery.com/abstracts/html/2013/90163ace/abstracts/bourg.htm" target="_blank">Bourget et al., 2013</a>
</p>
</div>
</div>
<div class="row">
<div class="col-xs-8 col-xs-offset-2"><br>
<img src="figures/delta.png" class="img-responsive img-centered" alt=""><br>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-left">
<p>
Download the delta <a href="examples/delta.tar" target="_blank">input files</a> (tarball).
</p>
<p>
<pre><code>folder: delta
specs: 227x145 cells, 400 m resolution, 30 kyrs
processes: uplift/subsidence + river + sea-level change
run duration: ~20 mn
</code></pre>
</p>
</div>
</div>
</div>
<div class="col-lg-12 text-center">
<hr class="star-primary">
</div>
</section>
<section id="ridge">
<div class="container">
<div class="row">
<div class="col-lg-12">
<h2>Ridge evolution</h2>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-left">
<p>
The Ridge example illustrates the impact of contrasting bedrock erodibility on drainage
development and sediment yielding during the evolution of a plateau to a ridge in a bedrock landscape,
under imposed climate and uplift.<br>
These two allogenic factors were set to represent a nonseasonal humid climate, with a mean annual rainfall
of 1500 mm, and a constant tectonic uplift rate of 5 mm/yr with a fixed-elevation boundary condition.
This fixed elevation boundary condition imposes a constant base-level but precludes the formation of a
piedmont at the base of the rising landscape.
</p>
</div>
</div>
<div class="row">
<div class="col-xs-8 col-xs-offset-2"><br>
<img src="figures/ridge.png" class="img-responsive img-centered" alt=""><br>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-left">
<p>
The experiment initial deposits is divided in a southern domain with non cohesive material and a northern one
with a basement material erodibility of 0.25.<br>
Download the ridge <a href="examples/ridge.tar" target="_blank">input files</a> (tarball).</p><p>
<pre><code>folder: ridge
specs: 401x151 cells, 50 m resolution, 30 kyrs
processes: uplift (5 mm/yr) + rain + mass movement
run duration: ~50 mn
</code></pre></p>
<p>
More <strong>Lecode</strong> simulations of the influence of contrasting bedrock erodibility on landscape dynamics
are available in the following submitted paper <a href="documents/EPSL.pdf" target="_blank">ESPL Submission</a>.
</p>
</div>
</div>
</div>
<div class="col-lg-12 text-center">
<hr class="star-primary">
</div>
</section>
<section id="s2s">
<div class="container">
<div class="row">
<div class="col-lg-12">
<h2>Source to sink model</h2>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-left">
<p>
The source-to-sink system comprises all areas that contribute to erosion, transportation and deposition of
sediments within an erosional-depositional system from catchment headwater to deep-marine basin floor fan.
</p>
</div>
</div>
<div class="row">
<div class="col-xs-8 col-xs-offset-2 text-center">
<div class="js-video [vimeo, widescreen]">
<iframe width="640" height="360" src="//www.youtube.com/embed/IY-9hDhDOuc?rel=0" frameborder="0" allowfullscreen></iframe>
</div>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-center">
<p>Example of Lecode source-to-sink experiments</p>
</div>
</div>
<!--div class="row">
<div class="col-xs-8 col-xs-offset-2 text-center"><br>
<img src="figures/s2s.png" class="img-responsive img-centered" alt=""><br>
<p>Initial setting for Lecode source-to-sink cookbook example</p>
</div>
</div-->
<div class="row">
<div class="col-lg-12 text-left">
<p>
Download the source to sink <a href="examples/src2sk.tar" target="_blank">input files</a> (tarball).</p><p>
<pre><code>folder: src2sk
specs: 298x314 cells, 250 m resolution, 500 yrs
processes: rain + mass movement
run duration: ~15 mn
</code></pre></p>
<p>
The depositional pattern for Lecode source-to-sink cookbook example should be similar to the ones shown below.
</p>
</div>
</div>
<div class="row">
<div class="col-xs-8 col-xs-offset-2"><br>
<img src="figures/s2s-out.png" class="img-responsive img-centered" alt=""><br>
</div>
</div>
</div>
<div class="col-lg-12 text-center">
<hr class="star-primary">
</div>
</section>
<section id="rift">
<div class="container">
<div class="row">
<div class="col-lg-12">
<h2>Rift sedimentation</h2>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-left">
<p>
One of the <strong>SGFM</strong> developments effort is around the deformation of the lithosphere at intermediate time-scales and interlinks with surface evolution. <br>
To study the nature of the interferences between dynamic topography, sediment transport/erosion, and
lithosphere instabilities, the <a href="https://www.underworldproject.org target="_blank">Underworld</a> model has been coupled to Lecode.
</p>
</div>
</div>
<div class="row">
<div class="col-xs-8 col-xs-offset-2"><br>
<img src="figures/udw-sgfm.png" class="img-responsive img-centered" alt=""><br>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-left">
<p>
The application is part of a larger project on <i>stratigraphic modelling of continental rifting</i>.
To get a detail information on the coupling technique and the full example results, see
<a href="http://adsabs.harvard.edu/abs/2013EGUGA..15.6616M" target="_blank">Mondy et al., 2013</a>.
<br>
<br>
The full model presents an oblique rifting with heterogeneous sub-continental lithospheric mantle.
Two cratons of differing rheologies are rifted apart at 1cm/yr on each boundary.
Here, the provided example uses the displacement fields generated by Underworld and there is no
coupling and consequently no feedback mechanisms between geodynamics and surface processes.
</p>
</div>
</div>
<!--div class="row">
<div class="col-xs-8 col-xs-offset-2"><br>
<img src="figures/rift.png" class="img-responsive img-centered" alt=""><br>
</div>
</div-->
<div class="row">
<div class="col-xs-8 col-xs-offset-2 text-center">
<div class="js-video [vimeo, widescreen]">
<iframe width="640" height="360" src="//www.youtube.com/embed/VPPXzd6kNaM?rel=0" frameborder="0" allowfullscreen></iframe>
<br>
</div>
</div>
</div>
<!--div class="row">
<div class="col-xs-8 col-xs-offset-2 text-center">
<div class="js-video [vimeo, widescreen]">
<iframe width="640" height="360" src="//www.youtube.com/embed/wn_IKqcOzhQ?rel=0" frameborder="0" allowfullscreen></iframe>
<br>
</div>
</div>
</div-->
<div class="row">
<div class="col-lg-12 text-center">
<p>
Example of models ran by Luke Mondy in 2013 to illustrate the <code>vertical only</code> coupling mediator technique.
</p>
</div>
</div>
<div class="row">
<div class="col-lg-12 text-left">
<p><br>
Download the rift <a href="examples/rift.tar" target="_blank">input files</a> (tarball).
<pre><code>folder: rift
specs: 161x161 cells, 1875 m resolution, 150 kyrs
processes: uplift/subsidence + rain + mass movement
run duration: ~25 mn
</code></pre> </p>
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