Excursion to the Czech part of Moldanubia, Tectometamorphic evolution of the Moldanubian zone near Jemnice (SOUTH MORAVIA, BOHEMIAN MASSIF)

Abstract

Roks in the studied area belong to the Gfohl unit of the Moravian part of the Moldanubian zone. The Gfohl unit, first described in Austria as the Gfohl nappe ( FUCHS and Matura 1976, TOLLMANN 1982), is composed of para- and orthogneiss