Record details

    Petrogenesis of the Variscan Granites in the Western Part of Bohemian Massif
Statement of responsibility
    Miloš René
Other titles
    Petrogeneze variských granitů západní části Českého masivu
    René, Miloš
Source title - serial
    Acta montana. Series A, Geodynamics
    Vol. 15
    s. 67-83
    1 obr., 10 diagr., 2 tab.
    České resumé
    Obsahuje bibliografické odkazy
    Zkr. název ser.: Acta montana (Praha), Ser. A.
Subject group
    asociace magmatická
    chemismus hornin
    diferenciace magmatická
    kontrola tektonická
    krušnohorský pluton
    vrásnění variské
    západočeský pluton
Geographical name
Abstract (in english)
   Variscan granitoids of the western part of the Bohemian Massif are represented by three groups of granitoids which differ in their age, texture, mineral and chemical composition. The oldest group is represented by a suite of metaluminous granodiorites to diorites and is the precursor of the younger metaluminous/peraluminous granites. The remaining two groups of monzogranites comprise magmatic suites described by gradual increase of the Rb/Zr, Rb/Ba and U/Th ratios and decrease of the LREE/HREE ratios. The most plausible model for the genesis of granitoids in the western part of the Bohemian Massif is the one of an oblique collision of single blocks of the earth crust along the West Bohemian shear zone and subsequent thickening of the earth crust in this area
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
Entered date
    5. 3. 2007
Import date
    8. 8. 2012