新疆火烧云超大型非硫化物铅锌矿床:发生表生氧化的密西西比河谷型矿床

吴志旖; 宋玉财; 侯增谦; 刘英超; 庄亮亮

doi:10.3799/dqkx.2018.358

Volume 44 Issue 6

Jun. 2019

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Wu Zhiyi, Song Yucai, Hou Zengqian, Liu Yingchao, Zhuang Liangliang, 2019. The World-Class Huoshaoyun Nonsulfide Zinc-Lead Deposit, Xinjiang, NW China: Formation by Supergene Oxidization of a Mississippi Valley-Type Deposit. Earth Science, 44(6): 1987-1997. doi: 10.3799/dqkx.2018.358

Citation:

Wu Zhiyi, Song Yucai, Hou Zengqian, Liu Yingchao, Zhuang Liangliang, 2019. The World-Class Huoshaoyun Nonsulfide Zinc-Lead Deposit, Xinjiang, NW China: Formation by Supergene Oxidization of a Mississippi Valley-Type Deposit. Earth Science, 44(6): 1987-1997. doi: 10.3799/dqkx.2018.358

Citation:

Wu Zhiyi, Song Yucai, Hou Zengqian, Liu Yingchao, Zhuang Liangliang, 2019. The World-Class Huoshaoyun Nonsulfide Zinc-Lead Deposit, Xinjiang, NW China: Formation by Supergene Oxidization of a Mississippi Valley-Type Deposit. Earth Science, 44(6): 1987-1997. doi: 10.3799/dqkx.2018.358

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The World-Class Huoshaoyun Nonsulfide Zinc-Lead Deposit, Xinjiang, NW China: Formation by Supergene Oxidization of a Mississippi Valley-Type Deposit

doi: 10.3799/dqkx.2018.358

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2018-08-28
Publish Date: 2019-06-15

Abstract

Abstract

Huoshaoyun is a newly discovered world-class nonsulfide zinc-lead deposit in Xinjiang, NW China, so its genesis attracts many geologists'attentions. Conformable orebodies in the deposit contain massive and minor stratiform and breccia-hosted ores that are dominated by smithsonite and cerussite. Ores are hosted by Middle Jurassic sedimentary gypsum-bearing platform facies carbonate. Clearly, the carbonate is typical host for Mississippi Valley-type (MVT) deposit rather than for sedimentary exhalative (SEDEX) deposit. Galena is common in the ores and was replaced by cerussite, implying that precursor mineralization in the deposit was zinc and lead sulfides. δ³⁴S_V-CDT values of the galena range from -34‰ to -18‰, indicating that derivation of reduced sulfur was related to bacterial sulfate reduction (BSR) process, which is common in MVT deposits but is scarce in magmatic -related Zn -Pb deposits. Together with the absence of magmatic -related hydrothermal alteration and mineralization, it suggests that primary mineralization at Huoshaoyun is of MVT origin. Oxygen isotopic compositions of water that reached isotopic equilibrium with smithsonite and cerussite are low in temperature and light in δ¹⁸O values, implyimg that meteoric water was involved in the two mineral formations. Combined with the observation that galena was replaced by cerussite, we suggest that the smithsonite and cerussite were the result of intensive supergene oxidization of primary znic and lead sulfides of MVT origin.
- smithsonite,
- cerussite,
- galena,
- platform carbonate,
- Mississippi Valley-type,
- supergene oxidization,
- Huoshaoyun,
- deposits

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The World-Class Huoshaoyun Nonsulfide Zinc-Lead Deposit, Xinjiang, NW China: Formation by Supergene Oxidization of a Mississippi Valley-Type Deposit

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