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The Saxo-Danubian granite belt: magmatic response to postcollisional delamination of mantle lithosphere the south-western sector of the Bohemian Massif (Variscan orogen)

  1. 1.
    SYSNO ASEP0330965
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleThe Saxo-Danubian granite belt: magmatic response to postcollisional delamination of mantle lithosphere the south-western sector of the Bohemian Massif (Variscan orogen)
    TitleSasko-dunajské granitové pásmo: magmatická odezva postkolizní delaminace plášťové litosféry pod jihozápadní částí Českého masívu (variský orogén)
    Author(s) Finger, F. (AT)
    Gerdes, A. (DE)
    René, Miloš (USMH-B) RID, ORCID, SAI
    Riegler, G. (AT)
    Source TitleGeologica Carpathica. - : Slovenská akadémia vied - ISSN 1335-0552
    Roč. 60, č. 3 (2009), s. 205-212
    Number of pages8 s.
    Languageeng - English
    CountrySK - Slovakia
    KeywordsBohemian Massif ; granite ; delamination
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsMEB060802 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    CEZAV0Z30460519 - USMH-B (2005-2011)
    UT WOS000268017900002
    AnnotationBased on the synchronicity of geochronological data and the similarity of granite types, it is proposed that the Erzgebirge Batholith in the Saxothuringian Zone and the South Bohemian Batholith in the Moldanubian Zone belong to one cogenetic plutonic megastructure.
    WorkplaceInstitute of Rock Structure and Mechanics
    ContactIva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
    Year of Publishing2010
Number of the records: 1  

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