SLOBODNÍK, Marek and Zdenek DOLNÍČEK. Hydrothermal mineralization beneath the Upper Silesian basin, Czech Republic: The record of a possible tectonic driving fluid flow. Geolines. Praha: AVČR, 2001, vol. 13, No 1, p. 109-110. ISSN 1210-9606.
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Basic information
Original name Hydrothermal mineralization beneath the Upper Silesian basin, Czech Republic: The record of a possible tectonic driving fluid flow
Authors SLOBODNÍK, Marek and Zdenek DOLNÍČEK.
Edition Geolines, Praha, AVČR, 2001, 1210-9606.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Czech Republic
Confidentiality degree is not subject to a state or trade secret
RIV identification code RIV/00216224:14310/01:00004806
Organization unit Faculty of Science
Keywords in English Upper Silesian Basin; faults; sulphides; calcite; fluid inclusions; stable isotopes
Tags calcite, faults, fluid inclusions, Stable Isotopes, sulphides, Upper Silesian Basin
Changed by Changed by: doc. RNDr. Marek Slobodník, CSc., učo 2488. Changed: 30/11/2001 14:50.
Abstract
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.
Links
GA205/00/0356, research and development projectName: Geochemický a tektonický model migrace fluid v paleozoiku moravskoslezské oblasti
Investor: Czech Science Foundation, Geochemical and tectonic model of fluid migration in the paleozoic of Moravo-Silesian region
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