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Remnants of Early Carboniferous I-type granodiorite plutons in the Bavarian Forest and their bearing on the tectonic interpretation of the south-western sector of the Bohemian Massif (Bavarian Zone)
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SYSNO ASEP 0356172 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Remnants of Early Carboniferous I-type granodiorite plutons in the Bavarian Forest and their bearing on the tectonic interpretation of the south-western sector of the Bohemian Massif (Bavarian Zone) Author(s) Finger, F. (AT)
Dunkley, D. J. (JP)
René, Miloš (USMH-B) RID, ORCID, SAISource Title Journal of Geosciences. - : Česká geologická společnost - ISSN 1802-6222
Roč. 55, č. 4 (2010), s. 321-332Number of pages 12 s. Publication form www - www Language eng - English Country CZ - Czech Republic Keywords granodiorite ; U-Pb dating ; Moldanubian Zone Subject RIV DB - Geology ; Mineralogy R&D Projects ME10083 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) CEZ AV0Z30460519 - USMH-B (2005-2011) UT WOS 000286342300002 DOI 10.3190/jgeosci.080 Annotation Occurrence of Hbl-bearing diatexite from the Bavarian Zone corresponds by its age and geochemistry exactly with granodiorites of the Blatná suite in the Central Bohemian I-type plutonic complex. Analyses on oscillatory-zoned zircon yield an age of 344 ± 2 Ma, interpreted as the formation age of the igneous protolith. Workplace Institute of Rock Structure and Mechanics Contact Iva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216 Year of Publishing 2011
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