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GAO Yongbao, ZHAO Xinmin, ZHAO Xiaojian, LI Kan, TENG Jiaxin, YAN Zhouquan, JIN Moushun, ZHAO Huibo. 2020. Mineralogy, Geochemistry and Genesis of Duobaoshan Zn-Pb Deposit, in Karakoram, Xinjiang. Northwestern Geology, 53(1): 122-137. doi: 10.19751/j.cnki.61-1149/p.2020.01.011
Citation: GAO Yongbao, ZHAO Xinmin, ZHAO Xiaojian, LI Kan, TENG Jiaxin, YAN Zhouquan, JIN Moushun, ZHAO Huibo. 2020. Mineralogy, Geochemistry and Genesis of Duobaoshan Zn-Pb Deposit, in Karakoram, Xinjiang. Northwestern Geology, 53(1): 122-137. doi: 10.19751/j.cnki.61-1149/p.2020.01.011
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Mineralogy, Geochemistry and Genesis of Duobaoshan Zn-Pb Deposit, in Karakoram, Xinjiang

  • Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, Xi'an Center of China Geological Survey/Northwest China Center for Geoscience Innovation, Xi'an 710054, Shaanxi, China

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Received Date:  20 December 2019
Revised Date:  25 December 2019
    Abstract
  • Located in Karakoram of Xinjiang, the Duobaoshan lead-zinc deposit was formed in the limestones of the Cretaceous Tielongtan Formation, and was obviously controlled by structural fracture zones. The ore bodies are irregularly sac-like, vein-like, and lenticular-shape-like. It can be divided into three metallogenic stages:the early sulfide mineralization stage, the intermediate replacement mineralization stage and the late oxidation stage. The first stage is characterized by galena, sphalerite and calcite; the second stage is represented by smithsonite, iron oxide, cerussite, and gypsum; the last stage is characterized by hydrozincite. The δ34S values of the galena in the first stage range from -14‰ to -0.6‰, which shows a feature of reduced sulfur source. The lead isotope compositions are concentrated and show a crustal source feature, and the Permian-Cretaceous sedimentary rocks may be the sources of metals. The δ18CPDB values of calcite are from 3.5‰ to 5.7‰ and the δ18OSMOW, from 22.1‰ to 27.1‰ are which indicate the dissolution of carbonate. The δ18CPDB and δ18OSMOW values of the smithsonite are from 2.9‰ to 3.8‰ and 16.9‰ to 20.3‰, respectively. The δ18CPDB and δ18OSMOW values of the cerussite are from 2.7‰ to 4.4‰ and 15.8‰ to 20.3‰, respectively. All these values indicate the mixing of atmospheric precipitation. The 3He/4He and 40Ar/36Ar ratios of the fluid inclusions in the calcite are from 0.72 R/Ra to 0.93 R/Ra and 302.1 to 350.7, respectively; and the 3He/4He and 40Ar/36Ar ratios of the fluid inclusions in the galena are 1.17 R/Ra and 298.1, respectively. The 3He/4He and 40Ar/36Ar ratios of fluid inclusions in the smithsonite are from 0.22R/Ra to 0.46R/Ra and 292.6 to 295.8, respectively; the 3He/4He and 40Ar/36Ar ratios of fluid inclusions in cerussite are from 0.40R/Ra to 0.59R/Ra and 292.9 to 295.4, respectively. Thus, the ore-forming fluid may be the crustal fluid mixed with atmospheric precipitation. In summary, the Duobaoshan zinc-lead deposit is the product of fold thrust in the edge of the basin, structural fluids and secondary replacement system. The sulfides are formed of structural fluids, and the nonsulfides are the result of direct replacement, with oxidation occurring and hydrozincites formed at the last stage.
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