The Eocene bimodal Piranshahr massif of the Sanandaj-Sirjan Zone, NW Iran: a marker of the end of the collision in the Zagros orogen
Loading...
Date
Authors
Mazhari, S.A.
Bea, F.
Amini, S.
Ghalamghash, J.
Molina, J.F.
Montero, P.
Scarrow, J.H.
Williams, Ian
Journal Title
Journal ISSN
Volume Title
Publisher
Geological Society of London
Abstract
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
Description
Citation
Collections
Source
Journal of the Geological Society
Type
Book Title
Entity type
Access Statement
License Rights
Restricted until
2037-12-31
Downloads
File
Description