Mineralogy and skarnification processes at the Avan Cu-Fe Skarn, northeast of Kharvana, NW Iran

Introduction The Avan Cu-Fe skarn is located at the southern margin of Qaradagh batholith, about 60 km north of Tabriz. The Skarn-type metasomatic alteration is the result of Qaradagh batholith intrusion into the Upper Cretaceous impure carbonates. The studied area belongs to the Central Iranian st...

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Bibliographic Details
Main Authors: Mir Ali Asghar Mokhtari, Mohammad Ebrahimi, Mohammad Reza Ghorbani
Format: Article
Language:fas
Published: Ferdowsi University of Mashhad 2017-02-01
Series:Journal of Economic Geology
Subjects:
Online Access:http://econg.um.ac.ir/index.php/econg/article/view/37548