Detailed Information on Publication Record
2001
Zn-Pb-Cu mineralization in reef carbonates beneath the Upper Silesian Basin, Czech Republic: possible extremity of the Silesian-Cracow MVT district
SLOBODNÍK, Marek, Philippe MUCHEZ and Zdenek DOLNÍČEKBasic 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
Language
English
Type of outcome
Stať ve sborníku
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/00216224:14310/01:00004807
Organization unit
Faculty of Science
ISBN
90-2651-846-3
Keywords in English
Carboniferous; limestones; mineralizing fluids; fluid inclusions; stable isotopes
Tags
International impact, Reviewed
Změněno: 5/1/2009 13:48, doc. RNDr. Marek Slobodník, CSc.
V originále
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.
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 project |
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