新疆东准噶尔库拉比也铜镍矿床含矿岩体的成因及构造意义: 年代学、岩石地球化学和Sr⁃Nd⁃Hf同位素证据

汤贺军; 孟贵祥; 王召林; 邓震; 李成文; 祁光; 薛融晖

doi:10.3799/dqkx.2022.128

Volume 47 Issue 9

Sep. 2022

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Article Navigation > Earth Science > 2022 > 47(9): 3192-3209

Tang Hejun, Meng Guixiang, Wang Zhaolin, Deng Zhen, Li Chengwen, Qi Guang, Xue Ronghui, 2022. Genesis and Tectonic Significance of Ore Bearing Rock Mass in Kulabiye Cu⁃Ni Deposit, East Junggar, Xinjiang: Evidence from Chronology, Geochemistry and Sr⁃Nd⁃Hf Isotopes. Earth Science, 47(9): 3192-3209. doi: 10.3799/dqkx.2022.128

Citation:

Tang Hejun, Meng Guixiang, Wang Zhaolin, Deng Zhen, Li Chengwen, Qi Guang, Xue Ronghui, 2022. Genesis and Tectonic Significance of Ore Bearing Rock Mass in Kulabiye Cu⁃Ni Deposit, East Junggar, Xinjiang: Evidence from Chronology, Geochemistry and Sr⁃Nd⁃Hf Isotopes. Earth Science, 47(9): 3192-3209. doi: 10.3799/dqkx.2022.128

Citation:

Tang Hejun, Meng Guixiang, Wang Zhaolin, Deng Zhen, Li Chengwen, Qi Guang, Xue Ronghui, 2022. Genesis and Tectonic Significance of Ore Bearing Rock Mass in Kulabiye Cu⁃Ni Deposit, East Junggar, Xinjiang: Evidence from Chronology, Geochemistry and Sr⁃Nd⁃Hf Isotopes. Earth Science, 47(9): 3192-3209. doi: 10.3799/dqkx.2022.128

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Genesis and Tectonic Significance of Ore Bearing Rock Mass in Kulabiye Cu⁃Ni Deposit, East Junggar, Xinjiang: Evidence from Chronology, Geochemistry and Sr⁃Nd⁃Hf Isotopes

doi: 10.3799/dqkx.2022.128

Tang Hejun^{1, 2
,
,},
Meng Guixiang^{1, 2
,
,
,},
Wang Zhaolin^{1, 2},
Deng Zhen^{1, 2},
Li Chengwen³,
Qi Guang^{1, 2},
Xue Ronghui^{1, 2}

1.
Chinese Academy of Geological Sciences, Beijing 100037, China
2.
China Deep Exploration Center⁃SinoProbe Center, China Geological Survey & Chinese Academy of Geological Sciences, Beijing 100037, China
3.
No. 2 Regional Geological Survey Team of the Xinjiang Bureau of Geology and Mineral Exploration and Development, Changji 831100, China

Received Date: 2022-04-08
Publish Date: 2022-09-25

Abstract

Abstract

Northern Xinjiang is the second largest Cu-Ni metallogenic area in China as an important part of the Central Asian Orogenic Belt with many mafic-ultramafic intrusions containing Cu-Ni sulfide. Kulabiye Cu-Ni deposit located in Fuyun County, Xinjiang is a new breakthrough in Cu-Ni prospecting in the northern margin of East Junggar after the largest Cu-Ni deposit (Kalatongke) in northern Xinjiang. Although the geological and geophysical characteristics of the deposit have been summarized and the genesis and prospecting criteria of deposit have been put forward in the previous studies, some key problems such as the genesis and tectonic significance of the ore bearing rock mass have not been solved. In this paper, the petrology, geochronology, chemistry and Sr-Nd-Hf isotope of Kulabiye ore bearing rock mass are studied. The ore bearing rock mass of Kulabiye Cu-Ni deposit are mainly gabbro. They show the right dipping pattern of LREE enrichment and HREE loss, enriched in LILE Ba, U and K, and depleted in HFSE Nb, Ta, Ti and Lu. The (⁸⁷Sr/⁸⁶Sr)_i of gabbro is 0.703 948-0.704 109, ε_Nd(t) is between 5.28 and 5.74, ¹⁷⁶Hf/¹⁷⁷Hf and ε_Hf(t) varies greatly, ranging from 0.282 851 to 0.283 034 and +8.6-+15.1. The average value of ε_Hf(t) is 12.9. Trace elements and Sr-Nd-Hf isotopes also show the addition of shell source materials in the source area. The formation age of the Kulabiye complex (about 278 Ma) is consistent with the mineralization age of the regional Cu-Ni deposit (about 300-270 Ma). The Kulabiye complex has probably been formed in a post collisional extensional environment, which is related to the upwelling of asthenosphere magma and the partial melting and magma mixing of the metasomatic mantle wedge. The diagenetic and metallogenic age of Kulabiye also reveals that magmatic activities related to Cu-Ni mineralization in the Early Permian occurred widely in the eastern Junggar area, and the northern margin of the eastern Junggar has superior Cu-Ni prospecting potential.
- Cu⁃Ni sulfide,
- Sr⁃Nd⁃Hf isotope,
- zircon U⁃Pb geochronology,
- post collisional extension,
- East Junggar,
- geochemistry

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References(95)

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