The Eocene bimodal Piranshahr Massif of the Sanadaj-Sirjan Zone, West Iran; a marker of the end of collision in the Zagros orogen @reply

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Bibliographic Details
Published in	Journal of the Geological Society Vol. 166; no. 5; pp. 983 - 984
Main Authors	Bea, F, Scarrow, J. H, Mazhari, S. A, Molina, J. F, Montero, P, Amini, S, Ghalamghash, J
Format	Journal Article
Language	English
Published	Geological Society of London 01.09.2009
Subjects	A-type granites age Arabian Plate Asia bimodal magmatism Cenozoic deformation Eocene Eurasian Plate extension felsic composition gabbros Geophysics granites igneous and metamorphic rocks igneous rocks intrusions Iran magmatism Middle East Paleogene peralkaline Petrology Piranshahr Massif plate collision plate tectonics plutonic rocks Sanandaj-Sirjan Zone solid Earth (tectonophysics) subduction syenites tectonics Tertiary Zagros
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ISSN:	0016-7649
DOI:	10.1144/0016-76492009-027