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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References(39)

References

Boni, M., Gilg, H. A., Balassone, G., et al., 2007. Hypogene Zn Carbonate Ores in the Angouran Deposit, NW Iran.Mineralium Deposita, 42, 799-820. doi: 10.1007/s00126-007-0144-4

Brugger, J., McPhail, D.C., Wallace, M., et al., 2003.Forma-tion of Willemite in Hydrothermal Environments. Eco-nomic Geology, 98(4):819-835. doi: 10.2113/gsecongeo.98.4.819

Dong, L. H., Xu, X. W., Fan, T. B., et al., 2015. Discovery of the Huoshaoyun Super-Large Exhalative-Sedimentary Carbonate Pb-Zn Deposit in the Western Kunlun Area and Its Great Significance for Regional Metallogeny.Xin-jiang Geology, 33(1):41-50(in Chinese with English ab-stract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xjdz2015010008

Fan, T.B., Yu, Y.J., Xia, M.Y., et al., 2017.Geological Fea-tures and Prospecting for the Huoshaoyun Pb-Zn Depos-it in Hotan, Xinjiang. Acta Geologica Sichuan, 37(4):578-582(in Chinese with English abstract).

Gao, Y.B., Teng, J.X., Li, K., et al., 2017.Metallogenic Char-acteristics and Genesis of the Huoshaoyun Superlarge Lead-Zinc Deposit in Karakorum.Acta Mineralogica Si-nica, 37(Suppl.):561-562(in Chinese).

Gilg, H.A., Boni, M., Hochleitner, R., et al., 2008.Stable Iso-tope Geochemistry of Carbonate Minerals in Supergene Oxidation Zones of Zn-Pb Deposits. Ore Geology Re-views, 33(2):117-133. doi: 10.1016/j.ore-georev.2007.02.005

Hitzman, M.W., 2003.Classification, Genesis, and Exploration Guides for Nonsulfide Zinc Deposits.Economic Geology, 98(4):685-714.doi: 10.2113/98.4.685

Hou, Z. Q., Cook, N. J., 2009. Metallogenesis of the Tibetan Collisional Orogen:A Review and Introduction to the Special Issue.Ore Geology Reviews, 36(1-3):2-24. doi: 10.1016/j.oregeorev.2009.05.001

Hou, Z.Q., Song, Y.C., Li, Z., et al., 2008.Thrust-Controlled, Sediments-Hosted Pb-Zn-Ag-Cu Deposits in Eastern and Northern Margins of Tibetan Orogenic Belt:Geolog-ical Features and Tectonic Model. Mineral Deposits, 27(2):123-144(in Chinese with English abstract).

Huang, Q.F., Lu, Y., 2016.Analysis of Geological Characteris-tics and Genesis of Hotan Huoshaoyun Lead-Zinc Depos-it. Resource Information and Engineeing, 31(4):3-5(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200904013.htm

Jin, H.Z., 2018.Analysis of Metallogenic Condition and Pros-pecting Potential of Lead-Zinc Deposit in Tianshuihai-Huoshaoyun Area, Karakoram. Journal of Geology, 42(1):17-22(in Chinese with English abstract).

Leach, D.L., Bradley, D.C., Huston, D., et al., 2010.Sediment-Hosted Lead-Zinc Deposits in Earth History. Economic Geology, 105:593-625. doi: 10.2113/gsec-ongeo.105.3.593

Leach, D.L., Sangster, D.F., Kelley, K.D., et al., 2005.Sedi-ment-Hosted Lead-Zinc Deposit:A Global Perspective.Economic Geology, 100:561-607.

Li, X.F., Zhang, M.J., Li, Y.J., et al., 2012.Characteristics of δ¹⁸O in Precipitation and Moisture Transports over the Arid Region in Northwest China.Environmental Science, 33(3):711-719(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hjkx201203006

Ohmoto, H., 1996. Formation of Volcanogenic Massive Sul-fide Deposits:The Kuroko Perspective.Ore Geology Re-views, 10(3-6):135-177. doi: 10.1016/0169-1368(95)00021-6

Ohmoto, H., Rye, R.O., 1979.Isotopes of Sulfur and Carbon. In: Barnes, H.L., ed., Geochemistry of Hydrothermal Ore Deposits.Wiley, New York, 509-567.

Reichert, J., Borg, G., 2008.Numerical Simulation and a Geo-chemical Model of Supergene Carbonate-Hosted Non-Sulphide Zinc Deposits. Ore Geology Reviews, 33(2):134-151. doi: 10.1016/j.oregeor-ev.2007.02.006

Song, Y. C., Hou, Z. Q., Liu, Y. C., et al., 2017. Mississippi Valley-Type (MVT) Pb-Zn Deposits in the Tethyan Do-main:A Review. Geology in China, 44(4):664-689(in Chinese with English abstract). doi: 10.1007/s001260100208

Song, Y. C., Hou, Z. Q., Yang, T. N., et al., 2011. Sediment-Hosted Himalayan Base Metal Deposits in Sanjiang Re-gion:Characteristics and Genetic Types.Acta Petrologi-ca et Mineralogica, 30(3):355-380(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201103003.htm

Spurlin, M. S., Yin, A., Horton, B. K., et al., 2005. Structural Evolution of the Yushu-Nangqian Region and Its Rela-tionship to Syncollisional Igneous Activity, East-Central Tibet. Geological Society of America Bulletin, 117(9):1293.doi: 10.1130/b25572.1

Taylor, H.P., 1974.The Application of Oxygen and Hydrogen Isotope Studies to Problems of Hydrothermal Alteration and Ore Deposition.Economic Geology, 69(6):843-883. doi: 10.2113/gsecongeo.69.6.843

Xiao, W.J., Li, J.L., Hou, Q.L., et al., 1998.Structural Styles of the Southeastern West Kunlun Mountains and Their Implication to Growing-Arc Orogenesis.Chinese Journal of Geophysics, 41(Suppl.):133-141(in Chinese with English abstract). http://cn.bing.com/academic/profile?id=8d30ed5707902d5032eb7b72d832176c&encoded=0&v=paper_preview&mkt=zh-cn

Yi, A., 2001. Geologic Evolution of the Himalayan-Tibetan Orogen in the Context of Phanerozoic Continental Growth of Asia.Acta Geoscientia Sinica, 22(3):193-230(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200103001

Zhang, Z.D., Zeng, Y.C., 1988.The Division and Evolution of Tectonic Area in Western Kunlun Mt.-Karakorum Mt.Xinjiang Geology, 6(1):60-72(in Chinese with English abstract). http://cn.bing.com/academic/profile?id=a903d0e17d7c8621c08b6d60b5f907fd&encoded=0&v=paper_preview&mkt=zh-cn

Zhao, D. D., Chen, H. L., Yang, S. F., et al., 2000. Structural Styles of the Foreland Fold and Thrust Belt in the Tians-huihai Area, Western Kunlun, and Its Tectonic Evolu-tion. Acta Geologica Sinica, 74(2):134-141(in Chinese with English abstract).

Zhou, M.L., Liu, Y.C., 2018.The Sachakou Deposit in West Kunlun of Xinjiang:A Pb-Zn Polymetallic Deposit Asso-ciated with Magmatic Metasomatism of Carbonate Rock.Acta Geologica Sinica(English Edition), 92(2):883-884.doi: 10.1111/1755-6724.13572

董连慧, 徐兴旺, 范廷宾, 等, 2015.喀喇昆仑火烧云超大型喷流-沉积成因碳酸盐型Pb-Zn矿的发现及区域成矿学意义.新疆地质, 33(1):41-50. doi: 10.3969/j.issn.1000-8845.2015.01.008

范廷宾, 余元军, 夏明毅, 等, 2017.新疆和田县火烧云铅锌矿地质特征及其找矿.四川地质学报, 37(4):578-582. doi: 10.3969/j.issn.1006-0995.2017.04.011

高永宝, 滕家欣, 李侃, 2017.喀喇昆仑火烧云超大型铅锌矿床成矿特征与成因.矿物学报, 37(增刊):561-562. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-KWXB201712001358.htm

侯增谦, 宋玉财, 李政, 等, 2008.青藏高原碰撞造山带Pb-Zn-Ag-Cu矿床新类型:成矿基本特征与构造控矿模型.矿床地质, 27(2):123-144. doi: 10.3969/j.issn.0258-7106.2008.02.001

黄清凤, 陆勇, 2016.新疆和田县火烧云铅锌矿地质特征及成因分析.资源信息与工程, 31(4):3-5. http://d.old.wanfangdata.com.cn/Periodical/ysjswz201604002

晋红展, 2018.喀喇昆仑甜水海-火烧云一带铅锌矿成矿条件及找矿潜力.地质学刊, 42(1):17-22. doi: 10.3969/j.issn.1674-3636.2018.01.003

李小飞, 张明军, 李亚举, 等, 2012.西北干旱区降水中δ¹⁸O变化特征及其水汽输送.环境科学, 33(3):711-719. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hjkx201203006

宋玉财, 侯增谦, 刘英超, 等, 2017.特提斯域的密西西比河谷型(MVT)铅锌矿床.中国地质, 44(4):664-689. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201704004

宋玉财, 侯增谦, 杨天南, 等, 2011. "三江"喜马拉雅期沉积岩容矿贱金属矿床基本特征与成因类型.岩石矿物学杂志, 30(3):355-380. doi: 10.3969/j.issn.1000-6524.2011.03.002

肖文交, 李继亮, 侯泉林, 等, 1998.西昆仑东南构造样式及其对增生弧造山作用的意义.地球物理学报, 41(增刊1):133-141. http://www.cnki.com.cn/Article/CJFDTotal-DQWX1998S1014.htm

尹安, 2001.喜马拉雅-青藏高原造山带地质演化:显生宙亚洲大陆生长.地球学报, 22(3):193-230. doi: 10.3321/j.issn:1006-3021.2001.03.001

张志德, 曾亚参, 1988.西昆仑山-喀喇昆仑山的构造分区及其演化.新疆地质, 6(1):60-67. http://www.cnki.com.cn/Article/CJFDTotal-XJDI198801005.htm

赵冬冬, 陈汉林, 杨树锋, 等, 2000.西昆仑甜水海地区前陆褶皱冲断带的构造样式及其演化.地质学报, 74(2):134-141. doi: 10.3321/j.issn:0001-5717.2000.02.005

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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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