Petrogenesis and geodynamic evolution of the Kajan Neogene subvolcanic rocks, Nain, Central Iran

tKajan subvolcanic rocks in the Urumieh–Dokhtar magmatic arc (UDMA), Central Iran, form a LateMiocene-Pliocene shallow-level intrusion. These subvolcanics correspond to a variety of intermediateand felsic rocks, comprising quartz diorite, quartz monzodiorite, tonalite and granite. These lithologies...

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Bibliographic Details
Main Author: Golkaram, S. (author)
Other Authors: Rashidnejad-Omran, N. (author), Azizi, H. (author), Asahara, Y. (author), Buchs, D. (author), McDonald. I. (author), Santos, J. F. (author)
Format: article
Language:eng
Published: 1000
Subjects:
Urumieh–Dokhtar magmatic arc (UDMA)
Magma differentiation
Sr and Nd isotope ratios
Calc-alkaline magmasa
Online Access:http://hdl.handle.net/10773/21150
Country:Portugal
Oai:oai:ria.ua.pt:10773/21150

Internet

http://hdl.handle.net/10773/21150

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