Geological characteristics and geochronology of the Takht-e-Gonbad copper deposit, SE Iran: A variant of porphyry type deposits
文献类型：期刊论文
| 作者 | Hosseini, Mohammad Reza1; Ghaderi, Majid1; Ahrezaei, Saeed2; Sun, Weidong3,4,5 |
| 刊名 | ORE GEOLOGY REVIEWS
 |
| 出版日期 | 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 |
| ISSN号 | 0169-1368 |
| 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. |
| WOS关键词 | U-PB GEOCHRONOLOGY ; MAGMATIC-HYDROTHERMAL FLUIDS ; CU-MO DEPOSIT ; STABLE-ISOTOPE ; ORE-DEPOSITS ; PHYLLIC ALTERATION ; SOUTHEASTERN IRAN ; GRANITIC-ROCKS ; NORTHERN CHILE ; EASTERN CHINA |
| WOS研究方向 | Geology ; Mineralogy ; Mining & Mineral Processing |
| 语种 | 英语 |
| WOS记录号 | WOS:000404064900025 |
| 出版者 | ELSEVIER SCIENCE BV |
| 资助机构 | Tarbiat Modares University of Iran ; National Science Foundation of China (NSFC)(91328204) |
| 源URL | [http://ir.qibebt.ac.cn/handle/337004/10457]  |
| 专题 | 中国科学院青岛生物能源与过程研究所 |
| 通讯作者 | Ghaderi, Majid |
| 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. |
入库方式： OAI收割
来源：青岛生物能源与过程研究所
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