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

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Authors	DOLNÍČEK Zdenek SLOBODNÍK Marek
Year of publication	2001
Type	Article in Periodical
Magazine / Source	Geolines
MU Faculty or unit	Faculty of Science
Citation
Field	Geology and mineralogy
Keywords	fluorite; REE; fluid inclusions; stable isotopes
Description	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, Jílové u Děčína).
Related projects:	Geochemical and tectonic model of fluid migration in the paleozoic of Moravo-Silesian region