Publication details

Podmínky vzniku hydrotermální kalcit-křemen-sulfidické mineralizace u Hranic

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Title in English Formation conditions of the calcite-quartz-sulphidic hydrothermal mineralization near Hranice
Authors

SLOBODNÍK Marek ZIMÁK Jiří DOLNÍČEK Zdeněk

Year of publication 2002
Type Article in Periodical
Magazine / Source Geol. Výzk. Mor. Slez. v r. 2001
MU Faculty or unit

Faculty of Science

Citation
Field Geology and mineralogy
Keywords devonian limestones; calcite veins; stable isotopes; fluid inclusions; basinal brines
Description There are numerous calcite veins with quartz and little sulphides that cut through the Devonian limestones near Hranice. They are assumed to be a post-Variscan mineralization stage. Low temperature fluids (50 to 100C), from which hydrothermal minerals precipitated, can be best interpreted as mainly basinal brines (type H2O-NaCl-CaCl2).
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