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Project Summary

Many tectonic problems require to treat the lithosphere as a compressible elastic material, which can also flow viscously or break in a brittle fashion depending on the stress level applied and the temperature conditions. We present a flexible methodology to address the resulting complex material response, which imposes severe challenges on the discretization and rheological models used. This robust, adaptive, two-dimensional, finite element method solves the momentum balance and the heat equation in Lagrangian form using unstructured meshes. An implementation of this methodology is released to the public with the publication of this paper and is named DynEarthSol2D.

http://onlinelibrary.wiley.com/doi/10.1002/jgrb.50148/abstract

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30 Day Summary

Jul 19 2020 — Aug 18 2020

12 Month Summary

Aug 18 2019 — Aug 18 2020

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