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Publisher © Czech Geological Survey, ISSN: 2336-5757 (online), 0514-8057 (print)

Lithological evolution of the Moldanubian paragneisses in the area between Čechtice and Jihlava

Miloš René

Geoscience Research Reports 34, 2001 (GRR for 2000), pages 105–107

Keywords: geochemistry, petrology, Moldanubian zone, Paragneiss

Map sheets: Ledeč nad Sázavou (23-12), Havlíčkův Brod (23-21), Jihlava (23-23)

Full text (PDF, 0.15 MB)

Abstract

Biotite and sillimanite-biotite paragneisses from the area between Čechtice and Jihlava originated by regional metamorphosis of claystones and greywackes. The origin by alteration of greywackes is characteristic mainly for quartzitic paragneisses. Distributions of trace elements (REE, Sr, Ti, Sc, Ni) indicate that acid calc-alkaline igneous rocks dominated in the source area of original sediments.