Thermo-mechanical role of a Cambro-Ordovician paleorift during the Variscan collision: the NE margin of the Bohemian Massif

Abstract

The tectonometamorphic model explains exhumation mechanism of a Cambro-Ordovician rift during Variscan collision (Bohemian massif). The model is based on petrological, geochronological and structural data and supported by thermo-rheological model.