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Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá-Barrandian unit-a correlation of U-Pb isotopic-dilution-TIMS ages (Bohemia, Czech Republic)

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    SYSNO ASEP0145543
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleNeoproterozoic to Early Cambrian history of an active plate margin in the Teplá-Barrandian unit-a correlation of U-Pb isotopic-dilution-TIMS ages (Bohemia, Czech Republic)
    Author(s) Dörr, W. (DE)
    Zulauf, G. (DE)
    Fiala, Jiří (GLU-S) SAI, RID
    Franke, W. (DE)
    Vejnar, Zdeněk (GLU-S) SAI
    Source TitleTectonophysics. - : Elsevier - ISSN 0040-1951
    Roč. 352, 1-2 (2002), s. 65-85
    Number of pages21 s.
    Languageeng - English
    CountryNL - Netherlands
    KeywordsU-Pb analyses ; Cadomian Orogeny ; Bohemian Massif
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsKSK3012103 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    KSK1012601 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    UT WOS000178358700004
    EID SCOPUS0037194506
    DOI10.1016/S0040-1951(02)00189-0
    AnnotationThe Neoproterozoic evolution of an active plate margin in the Teplá-Barrandian is similar to Avalonian rocks in Newfounland, whereas the Cambrian transtension and related calcalkaline plutons are reminiscent of the Cadomian Ossa-Morena Zone and the Armorican Massif in western Europe.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2003

Number of the records: 1  

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