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slab detachment benchmark #3068
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Looks good. If you accept all of the edits and squash, then we can merge!
doc/manual/manual.bib
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journal=epsl, | ||
volume={304}, | ||
number={}, | ||
pages={45-54}, |
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pages={45-54}, | |
pages={45--54}, |
doc/manual/manual.bib
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@@ -11490,4 +11490,67 @@ @book{jahu17 | |||
year={2017} | |||
} | |||
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@article{schm11, | |||
title={{A simple analytical solution for slab detachment}}, | |||
author={S.M. Schmalholz}, |
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author={S.M. Schmalholz}, | |
author={S. M. Schmalholz}, |
doc/manual/manual.bib
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@Article{hitg14, | ||
AUTHOR = {Hillebrand, B. and Thieulot, C. and Geenen, T. and van den Berg, A. P. and Spakman, W.}, | ||
TITLE = {Using the level set method in geodynamical modeling of multi-material flows and Earth's free surface}, |
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TITLE = {Using the level set method in geodynamical modeling of multi-material flows and Earth's free surface}, | |
TITLE = {Using the level set method in geodynamical modeling of multi-material flows and {E}arth's free surface}, |
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This benchmark is based on the setup by S. Schmalholtz \cite{schm11}, which was subsequently | ||
run with \aspect{} by A. Glerum \cite{gltf18}. | ||
The computational domain is a $1000 \text{km}\times 660 \text{km}$ box. |
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:-)
doc/manual/manual.tex
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\begin{figure} | ||
\centering | ||
\includegraphics[width=0.6\linewidth]{cookbooks/benchmarks/slab_detachment/drawing.png} | ||
\caption{Slab detachment benchmark: initial geometry |
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\caption{Slab detachment benchmark: initial geometry | |
\caption{Slab detachment benchmark: Initial geometry. |
doc/manual/manual.tex
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\end{figure} | ||
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Two materials are present in the domain: the lithosphere and the mantle as shown | ||
in Fig. (\ref{fig:slab_detachment_setup}). The gravity acceleration |
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in Fig. (\ref{fig:slab_detachment_setup}). The gravity acceleration | |
in Fig. \ref{fig:slab_detachment_setup}. The gravity acceleration |
doc/manual/manual.tex
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is Earth-like with $g=9.81 \text{m/s}^2$. | ||
The overriding plate is $80\text{km}$ thick and is placed at the top of the domain. | ||
The already subducted lithosphere extends vertically into the mantle for $250 \text{km}$. | ||
This slab has a density $\rho_s=3300\text{kg/m}^3$ and is characterised by a power-law flow law so that |
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This slab has a density $\rho_s=3300\text{kg/m}^3$ and is characterised by a power-law flow law so that | |
This slab has a density $\rho_s=3300\text{kg/m}^3$ and is characterized by a power-law flow law so that |
I have (hopefully) addressed all comments and squashed. |
In this cookbook (and I think others of yours), you never say where the files that implement the benchmark can be found. Take a look at how the other sections do that and if you wanted to fix this up in a follow-up, I'd gladly accept this! |
This is the setup and manual entry for the slab detachment benchmark that A. Glerum presented in Glerum et al 2018.