Geological characteristics and geochronology of the Takht-e-Gonbad copper deposit, SE Iran: A variant of porphyry type deposits

doi:10.1016/j.oregeorev.2017.03.003

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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 Reza 1; Ghaderi, Majid 1; Ahrezaei, Saeed 2; Sun, Weidong3,4,5
刊名	ORE GEOLOGY REVIEWS
	2017-06-01
卷号	86 页码:440-458
关键词	Urumieh-dokhtar Arc Kerman Belt Porphyry Copper Stable Isotope Fluid Inclusion Takht-e-gonbad Iran
DOI	10.1016/j.oregeorev.2017.03.003
文献子类	Article
英文摘要	The 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.
语种	英语
WOS记录号	WOS:000404064900025
内容类型	期刊论文
版本	出版稿
源URL	[http://ir.qdio.ac.cn/handle/337002/137122]
专题	海洋研究所_深海极端环境与生命过程研究中心
作者单位	1.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
推荐引用方式 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.