Calcite-andradite microclinite from Markvartice near Třebíč, western Moravia
Article PDFActa Mus. Moraviae, Sci. Nat. 75 (1990), issue 1–2, pages 29-40
Article
Abstract:
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.
Contact:
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
Citation:
Houzar, S., Šrein, V., 1990: Calcite-andradite microclinite from Markvartice near Třebíč, western Moravia. - Acta Mus. Moraviae, Sci. Nat., 75, 1-2, 29-40 (with Czech summary)Keywords:
alkali-feldspar gneiss, andradite, calcite, Czechoslovakia, metasomatite, microcline, Moldanubicum, tectonic lineISSN: 1211–8796