东天山黄山东和黄山西铜镍硫化物矿床含矿超镁铁岩的成岩-成矿作用机制：来自斜长石成分的约束

石煜; 王玉往; 王京彬; 周国超; 王海

doi:10.3799/dqkx.2022.136

Volume 47 Issue 9

Sep. 2022

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Article Navigation > Earth Science > 2022 > 47(9): 3244-3257

Shi Yu, Wang Yuwang, Wang Jingbin, Zhou Guochao, Wang Hai, 2022. Petrogenesis and Metallogenesis Mechanism of the Ore-Bearing Ultramafic Rocks from the Huangshandong and Huangshanxi Ni-Cu Sulfide Deposits, Eastern Tianshan: Constraints from Plagioclase Compositions. Earth Science, 47(9): 3244-3257. doi: 10.3799/dqkx.2022.136

Citation:

Shi Yu, Wang Yuwang, Wang Jingbin, Zhou Guochao, Wang Hai, 2022. Petrogenesis and Metallogenesis Mechanism of the Ore-Bearing Ultramafic Rocks from the Huangshandong and Huangshanxi Ni-Cu Sulfide Deposits, Eastern Tianshan: Constraints from Plagioclase Compositions. Earth Science, 47(9): 3244-3257. doi: 10.3799/dqkx.2022.136

Citation:

Shi Yu, Wang Yuwang, Wang Jingbin, Zhou Guochao, Wang Hai, 2022. Petrogenesis and Metallogenesis Mechanism of the Ore-Bearing Ultramafic Rocks from the Huangshandong and Huangshanxi Ni-Cu Sulfide Deposits, Eastern Tianshan: Constraints from Plagioclase Compositions. Earth Science, 47(9): 3244-3257. doi: 10.3799/dqkx.2022.136

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Petrogenesis and Metallogenesis Mechanism of the Ore-Bearing Ultramafic Rocks from the Huangshandong and Huangshanxi Ni-Cu Sulfide Deposits, Eastern Tianshan: Constraints from Plagioclase Compositions

doi: 10.3799/dqkx.2022.136

1.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
2.
Beijing Institute of Geology for Mineral Resources Co. Ltd., Beijing 100012, China
3.
Sino-Zijin Resources Ltd., Beijing 100012, China
4.
College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China

Received Date: 2022-04-12
Publish Date: 2022-09-25

Abstract

Abstract

The Huangshandong and Huangshanxi mafic-ultramafic intrusions in East Tianshan are products of regional large scale Early Permian mantle-derived magmatism, and host two large scale Ni-Cu sulfide deposits. Major ore reserves of the Huangshandong and Huangshanxi deposits are hosted in the ultramafic rocks. Therefore, petrogenesis of their ore-bearing ultramafic rocks plays key role in understanding the matallogenesis of the regional Ni-Cu sulfide deposits. This study uses back scattered electron (BSE) images to observe the ore-bearing ultramafic rocks from Huangshandong and Huangshanxi deposits, and find out that plagioclase phenocrysts show significant disequilibrium. EMPA was used to analyze the chemical compositions and chemical profiles of the plagioclase phenocrysts. The An value of plagioclase from Huangshandong and Huangshanxi ore-bearing ultramafic rocks varies from 48.6 to 75.6 and 44.9 to 79.2, respectively, suggesting that the parental magma of the ore-bearing ultramafic rocks had experienced significant composition change during emplacement. Combined with geology of these two deposits, it is proposed that addition of high differentiated mafic magma into low differentiated ultramafic magma significantly changed parental magma composition, leading to sulfide segregation and formation of the Huangshandong and Huangshanxi large scale Ni-Cu sulfide deposits.
- plagioclase,
- Ni-Cu sulfide deposits,
- mafic-ultramafic intrusion,
- Huangshandong,
- Huangshanxi,
- eastern Tianshan,
- mineral deposit

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References(88)

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