Simulating geodynamic processes is a challenging task because of the non-linearity and cross-scale nature of tectonic processes. A great challenge is the multispectral character of lithosphere deformation ranging from earthquake rupture (seconds) to tectonic evolution (Millions of years). At the same time, deformation mechanisms determined at the micro-scale (rock friction and crystal plasticity) are responsible for the motion and internal deformation of tectonic plates. This requires a …