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Alteration Geochemistry and Stable Isotope Insights Into Orogenic Gold Mineralization at the Zartorosht Deposit, Southeastern Iran
Author(s) -
Aliyari Farhang,
Rastad Ebrahim
Publication year - 2014
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.12375_19
Subject(s) - library science , citation , mineralization (soil science) , geochemistry , geology , computer science , soil science , soil water
The Zartorosht gold deposit, southern Sanandaj-Sirjan metamorphic belt, southeastern Iran, is hosted in highly strained, greenschist facies, late Paleozoic metabasalt and schist (Fig. 1). The orebodies are broadly parallel to the regional east-west-oriented normal faults, and the discordant mineralization comprises thick quartz-sulfide vein sets, small quartz-carbonate-sulfide veinlets, and enclosing hydrothermally altered host rocks.