Hydrothermal mineralization beneath the Upper Silesian basin, Czech Republic: The record of a possible tectonic driving fluid flow

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Authors

SLOBODNÍK Marek DOLNÍČEK Zdenek

Year of publication 2001
Type Article in Periodical
Magazine / Source Geolines
MU Faculty or unit

Faculty of Science

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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