A parallel, extensible finite element code to simulate convection in both 2D and 3D models.
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Updated
Jun 10, 2026 - C++
A parallel, extensible finite element code to simulate convection in both 2D and 3D models.
It is based on the thermal convection models of the Annulus Earth and shows a diagnostic heat-flux calculation. It also extends further to other planetary bodies by adding different physical parameters and setting up several planetary interior models.
A Python package for computing surface properties through geological time using plate tectonic reconstructions.
post-processing code for mantle convection numerical modeling results used in Choi and Foley (2024)
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