A Comment on „Two distinctive granite suites in SW Bohemian Massif and their record of emplacement: Constraints from geochemistry and Zircon 207Pb/206Pb geochronology“ by Siebel et al. Journal of Petrology 49, 1853-1872

0330964 - ÚSMH 2010 GB eng J - Článek v odborném periodiku
Finger, F. - René, Miloš
A Comment on „Two distinctive granite suites in SW Bohemian Massif and their record of emplacement: Constraints from geochemistry and Zircon 207Pb/206Pb geochronology“ by Siebel et al. Journal of Petrology 49, 1853-1872.
Journal of Petrology. Roč. 50, č. 4 (2009), s. 591-593. ISSN 0022-3530. E-ISSN 1460-2415
Grant CEP: GA MŠMT MEB060802
Výzkumný záměr: CEZ:AV0Z30460519
Klíčová slova: Bohemian Massif * Moldanubian Zone * granite
Kód oboru RIV: DB - Geologie a mineralogie
Impakt faktor: 3.738, rok: 2009

Presented geochemical data do not support model of Siebel et al. (2008), according to which the Bavarian Pfahl fault separates two regions of chemically distinct granite plutons. Furthermore, prominent pre-Variscan lithologies from north of the Pfahl fault continue in a SSW direction into the area south of the fault. This clearly refutes the idea that the Pfahl fault represents a terrane boundary in the plate tectonic sense.
Trvalý link: http://hdl.handle.net/11104/0176616