资源环境科技发展态势分析平台

Buoyancy forces associated with subducting lithosphere control the dynamics of convergent margins. In the post‐collisional stage these forces are significantly reduced, yet mountain building and seismicity are ongoing, albeit at lower rates. We leverage advances of a newly developed seismo‐thermo‐mechanical modeling approach to simulate tectonic and seismicity processes in a self‐driven subduction and continental collision setting. We demonstrate that the rearrangement of forces due to slab breakoff, in the post‐collisional stage, causes bending and rollback of the residual slab, suction forces and mantle traction at the base of the upper plate, while stress coupling transfers to the shallow crust. Our results provide an explanation for the post‐collisional evolution of the Central Alps, where the so‐called Slab Rollback Orogeny models explains the slow yet persistent upper plate advance, the height of the mountain range, and a seismicity pattern consistent with the different tectonic regimes throughout the orogen.