Geochemistry and petrogenesis of the Feshark intrusion (NE Isfahan city)

Geochemistry and petrogenesis of the Feshark intrusion (NE Isfahan city)

Introduction Granitic rocks are the most abundant rock types in various tectonic settings and they have originated from mantle-derived magmas and/or partial melting of crustal rocks. The Oligo-Miocene Feshark intrusion is situated in the northeast of the city of Isfahan, and a small part of Urumieh...

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Bibliographic Details
Main Authors:	Ali Kananian, Fatemeh Ghahramani, Fatemeh Sarjoughian, Jamshid Ahmadian, Kazem Kazemi
Format:	Article
Language:	fas
Published:	Ferdowsi University of Mashhad 2017-11-01
Series:	Journal of Economic Geology
Subjects:	intrusive rock petrogenesis tectonic setting Feshark Isfahan Urumieh Dokhtar arc
Online Access:	https://econg.um.ac.ir/index.php/econg/article/view/49676

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