Record details

Title
    Das Dohnaer Massif in der südöstlichen Elbezone
Statement of responsibility
    Friedrich Schust
Other titles
    Beiträge zum Grundgebirge in der Lausitz (Variant.)
Author
    Schust, Friedrich
Language
    německy
Source title - serial
    Geoprofil
Vol./nr.
    Jg. 10
Year
    2001
Notes
    5 obr., 3 tab., 2s. bibl.
    Anglické resumé
    il.
    Zkr. název ser.: Geoprofil
Subject group
    biotit
    datování K/Ar
    datování Pb/Pb
    granitoidy
    lineament
    lužický pluton
    mylonitizace
    vrásnění kadomské
    zirkon
Geographical name
    ČR-Čechy
    Dolní Žleb (Děčín)
    Rumburk (Děčín)
    SRN-Sachsen
Keyword
    Dohnaer
    Elbezone
    Massif
    Südöstlichen
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
Contributor
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
    U
Entered date
    27. 9. 2007
Import date
    8. 8. 2012