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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)
- 1.0356172 - ÚSMH 2011 RIV CZ eng J - Journal Article
Finger, F. - Dunkley, D. J. - René, Miloš
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).
Journal of Geosciences. Roč. 55, č. 4 (2010), s. 321-332. ISSN 1802-6222. E-ISSN 1803-1943
R&D Projects: GA MŠMT ME10083
Institutional research plan: CEZ:AV0Z30460519
Keywords : granodiorite * U-Pb dating * Moldanubian Zone
Subject RIV: DB - Geology ; Mineralogy
Impact factor: 1.026, year: 2010
www.jgeosci.org/index.php?pg=issue&vol=55&iss=4
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.
Permanent Link: http://hdl.handle.net/11104/0194766
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