Vertically Decoupled Thickening and Exhumation Processes in Orogenic Supra- and Infra-Structure During Building of Gemer-Vepor Continental Wedge

摘要

An abstract of an article examining plausible tectonic model explaining structural and metamorphic evolution of crustal levels most likely located between Gemer and Vepor interface is presented. It was found that this zone served as decoupling horizon separating vertically elevated rocks from those which were simultaneously buried.