Kalcit-andraditový mikroklinit z Markvartic u Třebíče na západní Moravě

Acta Mus. Moraviae, Sci. Nat. 75 (1990), vydání 1–2, stránky 29-40

Článek

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Abstrakt:

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.

Kontakt:

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

Citace

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)

Klíčová slova:

alkali-feldspar gneiss, andradite, calcite, Czechoslovakia, metasomatite, microcline, Moldanubicum, tectonic line

ISSN: 1211–8796