2001•Unpublished venueRequires access

The neoidic fluorite mineralization in the Brno massif: Interaction between fluid and rock

Zdeněk Dolníček, Marek Slobodník

Abstract

Fluorite mineralization from granitoids of the Brno massif has been studied. Hydrothermal minerals precipitated from low saline fluids at temperatures of 80-150C and they were shallow-circulating meteoric waters. Mineralization could be compared with the Tertiary fluorite mineralization in the North Bohemia region (Teplice, Jilove u Děcina).

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Available abstract

Key concepts: Fluorite, Mineralization (soil science), Massif, Geology, Geochemistry, Hydrothermal circulation, Meteoric water, Mineralogy