You are here:
Publication details
Podmínky vzniku hydrotermální kalcit-křemen-sulfidické mineralizace u Hranic
Title in English | Formation conditions of the calcite-quartz-sulphidic hydrothermal mineralization near Hranice |
---|---|
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). |
Related projects: |