Calcite-andradite microclinite from Markvartice near Třebíč, western MoraviaArticle PDF
Calcite-andradite microclinite from Markvartice near Třebíč, western Moravia
In the paper submitted, the basic geological, petrological and mineralogical data about calcite-andradite microclinites at Markvartice are presented. These rocks are a part of the Varied Group of the Moravian Moldanubicum and originated by metasomatism of gneisses and marbles along the tectonic line of the E-W direction.
Stanislav Houzar, West-Moravian Museum, Zámek 1, 674 01 Třebíč, Czechoslovakia
Vladimír Šrein, Institute of Geology and Geotechnics, Czechoslovak Acad. Sci., V Holešovičkách 41, 182 00, Praha 8, Czechoslovakia