Record details

Title
    Hydrothermal mineralization beneath the Upper Silesian basin, Czech Republic: The record of a possible tectonic driving fluid flow
Author
    Dolníček, Zdenek
    Slobodník, Marek
Language
    anglicky
Publication type
    článek v periodiku
Source title - serial
    Geolines
Vol./nr.
    Roč. 13, č. 1
Pages
    2
Year
    2001
Thesaurus term
    calcite
    faults
    fluid inclusions
    stable isotopes
    sulphides
    Upper Silesian Basin
Keyword
    Basin
    Beneath
    Czech
    Driving
    Flow
    Fluid
    Hydrothermal
    Mineralization
    Possible
    Record
    Republic
    Silesian
    Tectonic
    Upper
Abstract (in english)
   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.
Contributor
    MU Brno, Přírodovědecká fakulta
Contributor code
    MU, PřF
Source format
    R
Import date
    8. 8. 2012