Informace o publikaci
Hydrothermal mineralization beneath the Upper Silesian basin, Czech Republic: The record of a possible tectonic driving fluid flow
| Autoři | |
|---|---|
| Rok publikování | 2001 |
| Druh | Článek v odborném periodiku |
| Časopis / Zdroj | Geolines |
| Fakulta / Pracoviště MU | |
| Citace | |
| Obor | Geologie a mineralogie |
| Klíčová slova | Upper Silesian Basin; faults; sulphides; calcite; fluid inclusions; stable isotopes |
| Popis | A sulphide mineralization occured in Carboniferous limestones in several boreholes to the south of Ostrava. Hydrothermal solutions (Th between 55-156C) have been derived as basinal fluids. Main faults in the region are interpreted as a principal migration pathways and the implacement of the Carpathian nappes could be the common driving mechanism for migration of the mineralizing fluids. |
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