Publication details
Hydrothermal mineralization beneath the Upper Silesian basin, Czech Republic: The record of a possible tectonic driving fluid flow
| Authors | |
|---|---|
| Year of publication | 2001 |
| Type | Article in Periodical |
| Magazine / Source | Geolines |
| MU Faculty or unit | |
| Citation | |
| Field | Geology and mineralogy |
| Keywords | Upper Silesian Basin; faults; sulphides; calcite; fluid inclusions; stable isotopes |
| Description | 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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