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Imperial College London
- London, UK
Highlights
- Pro
Pinned Loading
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RHCW18_Plate_Model
RHCW18_Plate_Model PublicFinite difference scheme for calculating conductive cooling of oceanic lithosphere and associated changes in seafloor subsidence and heat flow.
Fortran 4
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optimal-regularisation
optimal-regularisation PublicForked from valentineap/optimal-regularisation
Python
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geodynamics/aspect
geodynamics/aspect PublicA parallel, extensible finite element code to simulate convection in both 2D and 3D models.
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