中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
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
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
DOI10.1111/1755-6724.14866
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
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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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