Variscan magnetic fabric overprinting in sedimentary and crystalline thrust sheets in the NE Bohemian Massif

A significant deformation exists in the Nizky Jesenik Mountains, which has carboniferous sedimentary rocks, and the Hruby Jesenik Mountains, which has Devonian crystalline and pre-Cambrian rocks. There is an overprinted magnetic fabric in the crystalline and sedimentary rocks. There is a ductile deformation due to slaty cleavage, as seen in the Andelska Hora formation and the Horni Benesov formation. A multistadial deformation development is exhibited by the Hruby Jesenik Mountains.