Podmínky vzniku hydrotermální kalcit-křemen-sulfidické mineralizace u Hranic
| Title in English | Formation conditions of the calcite-quartz-sulphidic hydrothermal mineralization near Hranice |
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| Authors | |
| Year of publication | 2002 |
| Type | Article in Periodical |
| Magazine / Source | Geol. Výzk. Mor. Slez. v r. 2001 |
| MU Faculty or unit | |
| 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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