Multi-scale modelling of the Rhine Graben Rift
We're exploring how tectonics across different scales influence geothermal potential in the Upper Rhine Graben. We use ASPECT (a geodynamic code) together with FastScape (a landscape evolution code) to build realistic fault-network histories, then connect those results to GOLEM (a thermo-hydro-mechanical modelling code) to simulate heat and fluid flow plus rock and fracture behavior. At each step, we compare model output with geological and geophysical observations to better guide geothermal drilling targets.