Description
The modified Spectral Finite Element Code (SFEC) is able to calculate the geoid signal of a 3D-density shell with a radial viscosity structure. The code determines the dynamic topography on the two free-slip surfaces, simulating mantle convection scenario on Mars. The scenario main file allows the user to link flexure code in the GSH repository with this modified version of SFEC to compute Martian mantle dynamics. The final data output are the dynamic topography of the top and bottom surfaces and the geoid signal related to the mass distribution.
| Date made available | 4 Oct 2024 |
|---|---|
| Publisher | TU Delft - 4TU.ResearchData |
| Date of data production | 2024 - |