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The Eocene bimodal Piranshahr massif of the Sanandaj-Sirjan Zone, NW Iran: a marker of the end of the collision in the Zagros orogen

Mazhari, S.A.; Bea, F.; Amini, S.; Ghalamghash, J.; Molina, J.F.; Montero, P.; Scarrow, J.H.; Williams, Ian


The bimodal Piranshahr massif is composed of coeval but geochemically unrelated mafic (40.7 ± 0.2 Ma zircon U-Pb sensitive high-resolution ion microprobe (SHRIMP) age) and A-type felsic rocks (41 ± 0.5 Ma Rb-Sr and 41.3 plusmn; 0.8 Ma zircon U-Pb SHRIMP

CollectionsANU Research Publications
Date published: 2009
Type: Journal article
Source: Journal of the Geological Society
DOI: 10.1144/0016-76492008-022


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