新疆北部VMS矿床地质特征及成矿规律

杨富全; 耿新霞; 武峰; 张志欣; 成曦晖; 张振龙; 李宁

doi:10.3799/dqkx.2021.118

Volume 47 Issue 9

Sep. 2022

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Article Navigation > Earth Science > 2022 > 47(9): 3147-3173

Yang Fuquan, Geng Xinxia, Wu Feng, Zhang Zhixin, Cheng Xihui, Zhang Zhenlong, Li Ning, 2022. VMS Deposits in the Northern Xinjiang: Geological Characteristics and Metallogeny. Earth Science, 47(9): 3147-3173. doi: 10.3799/dqkx.2021.118

Citation:

Yang Fuquan, Geng Xinxia, Wu Feng, Zhang Zhixin, Cheng Xihui, Zhang Zhenlong, Li Ning, 2022. VMS Deposits in the Northern Xinjiang: Geological Characteristics and Metallogeny. Earth Science, 47(9): 3147-3173. doi: 10.3799/dqkx.2021.118

Citation:

Yang Fuquan, Geng Xinxia, Wu Feng, Zhang Zhixin, Cheng Xihui, Zhang Zhenlong, Li Ning, 2022. VMS Deposits in the Northern Xinjiang: Geological Characteristics and Metallogeny. Earth Science, 47(9): 3147-3173. doi: 10.3799/dqkx.2021.118

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VMS Deposits in the Northern Xinjiang: Geological Characteristics and Metallogeny

doi: 10.3799/dqkx.2021.118

1.
Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources; Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
No.5 Geological Party of Hebei Bureau of Geology and Mineral Resources Exploration, Tangshan 063004, China
3.
Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
4.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
5.
College of Mining Engineering, Taiyuan University of Technology, Taiyuan 030024, China

Received Date: 2021-08-09
Publish Date: 2022-09-25

Abstract

Abstract

Volcanogenic massive sulfide (VMS) is one of the most important deposit types in the Central Asian Orogenic Belt (CAOB). In the CAOB in Xinjiang (northern Xinjiang), VMS deposits are mainly distributed in the Ashele, Kelan, Maizi, and Kalatag ore dense districts of the Altay and the East Tianshan. The orebodies occurr in marine volcanic sedimentary rocks from the Lower-Middle Silurian Hongliuxia Formation, the Upper Silurian-Lower Devonian Kangbutiebao Formation, the Lower-Middle Devonian Ashele Formation, and the Lower Carboniferous Xiaorequanzi Formation. Exhalation rocks are developed in these ore districts, such iron-bearing jasper rock, barite, siliceous rock, ferromanganese marble, pyrite layer, and chlorite rock. There are many mineralization types developed in VMS metallogenic system, including the "two-layered structure" (layered/lenticular type and vein type from recharge zone), vein type related to volcanic hydrothermal fluids, and disseminated/vein type associated with sub-volcanic hydrothermal fluids. The VMS deposits in Xinjiang formed in three metallogenic periods: the Early-Middle Silurian (428-438 Ma), the Early-Middle Devonian (379-413 Ma), and Early Carboniferous (332-359 Ma). Sulfur of these deposits is derived from the underlying volcanic rock, inorganic sulfate reduction of seawater, and bacterial sulfate reduction. Ore-forming fluids are characterized by medium-low temperature (300-120 ℃) and low salinity (2%-10% NaCl_eq), and are deep-circulation seawater mixed with magmatic water in different proportions. The VMS metallogenic system is affected by volcanic structure, lithofacies, mineralization type, ore-forming fluids source, and physical-chemical condition, which results in a complex combination of mineralization elements.
- mineral deposits,
- geological characteristics,
- VMS deposit,
- metallogeny,
- Central Asian Orogenic Belt,
- Xinjiang

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References(113)

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VMS Deposits in the Northern Xinjiang: Geological Characteristics and Metallogeny

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