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Geological characteristics and geochronology of the Takht-e-Gonbad copper deposit, SE Iran: A variant of porphyry type deposits
Hosseini, Mohammad Reza1; Ghaderi, Majid1; Ahrezaei, Saeed2; Sun, Weidong3,4,5
2017-06-01
Source PublicationORE GEOLOGY REVIEWS
Volume86Pages:440-458
SubtypeArticle
AbstractThe Takht-e-Gonbad, or simply Takht, copper deposit in the Kerman belt in southern section of the Cenozoic Urumieh-Dokhtar magmatic arc (UDMA) of Iran is spatially associated with late Oligocene shallow granodiorite porphyries intruded into pyroclastic rocks. Hypogene ore minerals include pyrite, chalcopyrite, magnetite and rare molybdenite and bornite, occurring as veinlets and disseminations mostly in the pyroclastic rocks. Hydrothermal alteration is marked by an extensive phyllic assemblage and irregular zones of propylitic and calc-silicate assemblages with no consistent zoning patterns. The various igneous rocks at Takht area are calc-alkaline to shoshonitic, and are distinguished by enrichments in LILEs relative to HFSEs, and LREEs relative to HREEs (14.41 >= La-N/Yb-N >= 2.85). These features suggest a subduction-related setting for the rocks and the associated copper deposit in the area. A late Oligocene age is obtained for the main Takht granodiorite porphyry and the granodiorite batholith (24.2 Ma and 25.0 Ma, respectively, zircon U-Pb). The age of the main Takht porphyry is distinctly older than the middle-late Miocene ages reported for most porphyry Cu deposits occurring to the north of the Takht deposit, including the world-class Sarcheshmeh and Meiduk.
KeywordUrumieh-dokhtar Arc Kerman Belt Porphyry Copper Stable Isotope Fluid Inclusion Takht-e-gonbad Iran
DOI10.1016/j.oregeorev.2017.03.003
Indexed BySCI
Language英语
WOS IDWOS:000404064900025
Citation statistics
Cited Times:5[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Version出版稿
Identifierhttp://ir.qdio.ac.cn/handle/337002/137122
Collection深海极端环境与生命过程研究中心
Affiliation1.Tarbiat Modares Univ, Dept Econ Geol, Tehran 14115175, Iran
2.Shahid Beheshti Univ, Fac Earth Sci, Tehran, Iran
3.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, Qingdao, Peoples R China
4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao, Peoples R China
5.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
Recommended Citation
GB/T 7714
Hosseini, Mohammad Reza,Ghaderi, Majid,Ahrezaei, Saeed,et al. Geological characteristics and geochronology of the Takht-e-Gonbad copper deposit, SE Iran: A variant of porphyry type deposits[J]. ORE GEOLOGY REVIEWS,2017,86:440-458.
APA Hosseini, Mohammad Reza,Ghaderi, Majid,Ahrezaei, Saeed,&Sun, Weidong.(2017).Geological characteristics and geochronology of the Takht-e-Gonbad copper deposit, SE Iran: A variant of porphyry type deposits.ORE GEOLOGY REVIEWS,86,440-458.
MLA Hosseini, Mohammad Reza,et al."Geological characteristics and geochronology of the Takht-e-Gonbad copper deposit, SE Iran: A variant of porphyry type deposits".ORE GEOLOGY REVIEWS 86(2017):440-458.
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