Geology mineralogy, structure and texture of Agh-Otagh base- precious metal mineralization (North Takab)
The Agh-Otagh mineralization area in the north of Takab, was formed within the andesistic tuffaceous rocks of the Oligo- Miocene age. Mineralization include polymetallic (Cu-Pb-Zn-Au-Ag) quartz veins and silicified zones, which occurred as breccia and vein- veinlets with comb, cockade and disseminat...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | fas |
| Published: |
University of Isfahan
2017-07-01
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| Series: | پترولوژی |
| Subjects: | |
| Online Access: | http://ijp.ui.ac.ir/article_21956_dc847953041ec3c18fdc049f358e0aa6.pdf |