Miloš René


The amphibolites from the Vícenice quarry are part of a larger body on the northwestern margin of the Náměšť nad Oslavou granulite body. According to their modal composition, the plagioclase-amphibolite and epidote amphibolite there occur. Amphibolites are a metamorphic equivalent of magnesium enriched tholeiite basalts with considerable signature of partly enriched middle ocean ridge basalts (E-MORB).

Bibliografická citace

René, M. (2016). GEOCHEMIE A PETROGRAFIE AMFIBOLITŮ Z VÍCENICKÉHO LOMU U NÁMĚŠTĚ NAD OSLAVOU. Geologické výzkumy na Moravě a ve Slezsku, 16. Získáno z

Klíčová slova

Moldanubian Zone; amphibolite; petrography; geochemistry; MORB

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