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

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.

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

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Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10500 1.5. Earth and related environmental sciences

Country of publisher

Czech Republic

Confidentiality degree

není předmětem státního či obchodního tajemství

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

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Abstract

V originále

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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Links

GA205/00/0356, research and development project

Name: 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