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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 ASEP 0145543 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title 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) Author(s) Dörr, W. (DE)
Zulauf, G. (DE)
Fiala, Jiří (GLU-S) SAI, RID
Franke, W. (DE)
Vejnar, Zdeněk (GLU-S) SAISource Title Tectonophysics. - : Elsevier - ISSN 0040-1951
Roč. 352, 1-2 (2002), s. 65-85Number of pages 21 s. Language eng - English Country NL - Netherlands Keywords U-Pb analyses ; Cadomian Orogeny ; Bohemian Massif Subject RIV DB - Geology ; Mineralogy R&D Projects KSK3012103 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 WOS 000178358700004 EID SCOPUS 0037194506 DOI 10.1016/S0040-1951(02)00189-0 Annotation The 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. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2003
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