Origin and evolution of the Masjed Daghi Cu-Au-Mo porphyry and gold epithermal vein system, NW Iran: constraints from fluid inclusions and sulfur isotope studies

被引:0
|
作者
Susan Ebrahimi
Yuanming Pan
Mahnaz Rezaeian
机构
[1] Shahrood University of Technology,Faculty of Mining Engineering, Petroleum and Geophysics
[2] University of Saskatchewan,Department of Geological Sciences
[3] Institute for Advanced Studies in Basic Sciences (IASBS),Department of Earth Sciences
来源
Mineralogy and Petrology | 2021年 / 115卷
关键词
Copper Porphyry; Gold Epithermal; Masjed Daghi; Arasbaran; Iran;
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学科分类号
摘要
The Masjed Daghi porphyry-epithermal Cu-Au-Mo deposit in the northern Arabian-Eurasian collision zone of the Alborz Magmatic Assemblage, NW Iran, is hosted by an early Miocene quartz monzodiorite to diorite intrusion that intruded Eocene volcanic rocks. Potassic, phyllic, argillic, and propylitic alterations associated with four stages of porphyry mineralization (I to IV) are distinguished. Late high-sulfidation epithermal veins of mainly quartz or quartz-barite are enclosed in concentric zones of advanced argillic, argillic, silicic, and propylitic alterations.
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页码:643 / 662
页数:19
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