Rhenium-Osmium Isotope Constraints on the Origin of the Tianyu Cu-Ni Deposit in the East Tianshan Orogenic Belt, Xinjiang, NW China
文献类型:期刊论文
作者 | Han, Chunming1,2; Xiao, Wenjiao1,2; Ao, Songjian1; Zhang, Jien1; Song, Dongfang1; Zhang, Zhiyong1; Song, Shuaihua1; Xie, Mingcai1 |
刊名 | ACTA GEOLOGICA SINICA-ENGLISH EDITION
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出版日期 | 2022-04-01 |
卷号 | 96期号:2页码:525-535 |
关键词 | rhenium-osmium isotope Cu-Ni deposit Tianyu intrusion East Tianshan orogenic belt Xinjiang |
ISSN号 | 1000-9515 |
DOI | 10.1111/1755-6724.14866 |
英文摘要 | The Tianyu Cu-Ni sulfide deposit occurs in the north margin of the Central Tianshan Arc in East Tianshan orogenic belt, Xinjiang, NW China. The intrusions consist of gabbro, peridotite, and olivine pyroxenite. The peridotite and pyroxenite are the main host rock for the Cu-Ni ores. Rhenium and osmium isotopic analyses of Ni- and Cu-bearing sulfide minerals from the deposit have been used to determine the source of osmium, and by inference, the sources of ore metals. Sulfide ore samples have Os and Re concentrations varying in the ranges 1.85 to 4.58 ppb and 93.56 to 146.00 ppb, respectively. An initial Os-187/Os-188 ratio ranges from 0.86 to 1.23 for the ores and the gamma Os values from 592 to 2227. Osmium isotopic data suggest that the Tianyu intrusion and associated Cu-Ni mineralization has derived from crustal-contaminated mantle melts. The intrusions early show island-arc geochemical signatures, which indicate that the Hulu mafic-ultramafic intrusions, along with the Cu-Ni deposit, formed as a result of subduction of oceanic crust in the Early Permian. |
WOS关键词 | MAFIC-ULTRAMAFIC INTRUSIONS ; RE-OS AGES ; SM-ND ; U-PB ; GEOCHEMICAL CHARACTERISTICS ; COLLISIONAL TECTONICS ; STILLWATER COMPLEX ; NORTHERN XINJIANG ; SULFIDE DEPOSIT ; MANTLE SOURCE |
资助项目 | Second Tibetan Plateau Scientific Expedition and Research Program[2019QZKK0801] ; National Key R&D Program of China[2021YFC2901704] |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000788236600011 |
出版者 | WILEY |
资助机构 | Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/105149] ![]() |
专题 | 地质与地球物理研究所_中国科学院矿产资源研究重点实验室 |
通讯作者 | Han, Chunming |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resource, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Xinjiang Res Ctr Mineral Resources, Urumqi 830011, Peoples R China |
推荐引用方式 GB/T 7714 | Han, Chunming,Xiao, Wenjiao,Ao, Songjian,et al. Rhenium-Osmium Isotope Constraints on the Origin of the Tianyu Cu-Ni Deposit in the East Tianshan Orogenic Belt, Xinjiang, NW China[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2022,96(2):525-535. |
APA | Han, Chunming.,Xiao, Wenjiao.,Ao, Songjian.,Zhang, Jien.,Song, Dongfang.,...&Xie, Mingcai.(2022).Rhenium-Osmium Isotope Constraints on the Origin of the Tianyu Cu-Ni Deposit in the East Tianshan Orogenic Belt, Xinjiang, NW China.ACTA GEOLOGICA SINICA-ENGLISH EDITION,96(2),525-535. |
MLA | Han, Chunming,et al."Rhenium-Osmium Isotope Constraints on the Origin of the Tianyu Cu-Ni Deposit in the East Tianshan Orogenic Belt, Xinjiang, NW China".ACTA GEOLOGICA SINICA-ENGLISH EDITION 96.2(2022):525-535. |
入库方式: OAI收割
来源:地质与地球物理研究所
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