Record details

Title
    Major and trace elements in pyrope?almandine garnets as sediment provenance indicators of the Lower Carboniferous Culm sediments, Drahany Uplands, Bohemian Massif
Other titles
    Major and trace elements in pyrope?almandine garnets as sediment provenance indicators of the Lower Carboniferous Culm sediments, Drahany Uplands, Bohemian Massif
Author
    Čopjaková, Renata
    Paterson, Bruce
    Sulovský, Petr
Language
    anglicky
Publication type
    článek v periodiku
Source title - serial
    Lithos
Vol./nr.
    Roč. 82, č. únor
Pages
    20
Year
    2005
Thesaurus term
    Garnet chemistry, Trace elements, Granulites, Lower Carboniferous Culm Basin, Provenance, Bohemian Massif
Keyword
    Bohemian
    Carboniferous
    Culm
    Drahany
    Elements
    Garnets
    Indicators
    Lower
    Major
    Massif
    Provenance
    Pyrope?almandine
    Sediment
    Sediments
    Trace
    Uplands
Abstract (in czech)
   The Lower Carboniferous Culm Basin is part of the European Variscan foreland basin. Garnet is an abundant heavy mineral at all stratigraphic levels of the Culm sediments (the Protivanov, Rozsta´n?´ and Myslejovice Formation from base to top). This paper compares the major element (electron microprobe) and trace element (LA-ICP-MS) compositions of garnet for the purpose of studying the provenance of the Culm sediments.
Abstract (in english)
   The Lower Carboniferous Culm Basin is part of the European Variscan foreland basin. Garnet is an abundant heavy mineral at all stratigraphic levels of the Culm sediments (the Protivanov, Rozsta´n?´ and Myslejovice Formation from base to top). This paper compares the major element (electron microprobe) and trace element (LA-ICP-MS) compositions of garnet for the purpose of studying the provenance of the Culm sediments.
Contributor
    Česká geologická služba
Contributor code
    ČGS (RIV)
Source format
    R
Import date
    15. 10. 2014