Record details

    Das Dohnaer Massif in der südöstlichen Elbezone
Statement of responsibility
    Friedrich Schust
Other titles
    Beiträge zum Grundgebirge in der Lausitz (Variant.)
    Schust, Friedrich
Source title - serial
    Jg. 10
    5 obr., 3 tab., 2s. bibl.
    Anglické resumé
    Zkr. název ser.: Geoprofil
Subject group
    datování K/Ar
    datování Pb/Pb
    lužický pluton
    vrásnění kadomské
Geographical name
    Dolní Žleb (Děčín)
    Rumburk (Děčín)
Abstract (in english)
   The granitoids of the prevariscian Dohna Massif in the southeastern Elbe zone are part of the postkinematik cadomic-cambro-ordovizian granodiorit-complex of Lusatia and the Iser Montains. Southest of the Lusatian Fault - the boundary between the Elbe zone and the Lusatian antiklinal zone - the basement of the Elbe zone is covered with younger sediments, below which the Dohna granitoids spread out several times in the river valleys. In the Southwest the granitoids ere intrusively on the youngproterozoic grayackes of Weesenstein and Dolní Žleb (Niedergrund, Rasseln - north of Děčín, Czech Republic). In the northwestern Elbe zone the substantially lineamentspecific variscan Meissen Massif separates the proterozoic-cadomic Greywacke-granitoid-complexes of Weesenstein-Dohna and Clanzschitz-Laas
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
Entered date
    27. 9. 2007
Import date
    8. 8. 2012