SLOBODNÍK, Marek, Philippe MUCHEZ and Zdenek DOLNÍČEK. Zn-Pb-Cu mineralization in reef carbonates beneath the Upper Silesian Basin, Czech Republic: possible extremity of the Silesian-Cracow MVT district. In A.Piestrzynski et al.: Mineral deposits at the beginning of the 21st century. Amsterodam: A.A.Balkema Publishers, 2001, p. 209-212. ISBN 90-2651-846-3.
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Basic information
Original name Zn-Pb-Cu mineralization in reef carbonates beneath the Upper Silesian Basin, Czech Republic: possible extremity of the Silesian-Cracow MVT district
Authors SLOBODNÍK, Marek (203 Czech Republic, guarantor), Philippe MUCHEZ and Zdenek DOLNÍČEK.
Edition Amsterodam, A.Piestrzynski et al.: Mineral deposits at the beginning of the 21st century, p. 209-212, 2001.
Publisher A.A.Balkema Publishers
Other information
Original language English
Type of outcome Proceedings paper
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/00216224:14310/01:00004807
Organization unit Faculty of Science
ISBN 90-2651-846-3
Keywords in English Carboniferous; limestones; mineralizing fluids; fluid inclusions; stable isotopes
Tags Carboniferous, fluid inclusions, limestones, mineralizing fluids, Stable Isotopes
Tags International impact, Reviewed
Changed by Changed by: doc. RNDr. Marek Slobodník, CSc., učo 2488. Changed: 5/1/2009 13:48.
Abstract
Hydrothermal mineralization with sphalerite, galena, chalcopyrite, pyrite and marcasite occurs in massive reef carbonates of early Carboniferous age, beneath the Upper Carboniferous coal-bearing sediments of the Upper Silesian Basin. During precipitation of the successive mineral generations, temperature, salinity and composition of the mineralizing fluids changed. The physico-chemical characteristics of mineral precipitation indicate a comparable origin to the Mississippi Valley type deposits in Poland.
Abstract (in Czech)
Hydrothermal mineralization with sphalerite, galena, chalcopyrite, pyrite and marcasite occurs in massive reef carbonates of early Carboniferous age, beneath the Upper Carboniferous coal-bearing sediments of the Upper Silesian Basin. During precipitation of the successive mineral generations, temperature, salinity and composition of the mineralizing fluids changed. The physico-chemical characteristics of mineral precipitation indicate a comparable origin to the Mississippi Valley type deposits in Poland.
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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