Record details

Title
    Zn-Pb-Cu mineralization in reef carbonates beneath the Upper Silesian Basin, Czech Republic: possible extremity of the Silesian-Cracow MVT district
Author
    Dolníček, Zdenek
    Muchez, Philippe
    Slobodník, Marek
Language
    anglicky
Publication type
    článek ve sborníku
Source title - monograph
    A.Piestrzynski et al.: Mineral deposits at the beginning of the 21st century
Pages
    4
Notes
    Akce: 2001 ; 26-29 August 2001, Cracow, Poland
Thesaurus term
    Carboniferous
    fluid inclusions
    limestones
    mineralizing fluids
    stable isotopes
Keyword
    Basin
    Beneath
    Carbonates
    Czech
    District
    Extremity
    Mineralization
    MVT
    Possible
    Reef
    Republic
    Silesian
    Silesian-Cracow
    Upper
    Zn-Pb-Cu
Abstract (in english)
   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.
Contributor
    MU Brno, Přírodovědecká fakulta
Contributor code
    MU, PřF
Source format
    R
Import date
    8. 8. 2012