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    Volume 36 Issue 2
    Mar.  2011
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    Article Navigation >  Earth Science  > 2011  >  36(2): 277-281
    CHEN Shou-yu, ZHAO Peng-da, TONG Xiang, WU Jun-de, MO Guo-pei, CHEN Xing-shou, 2011. Metallogenic Characteristics of Western Low Altered Tin-Copper Polymetallic Deposit and Its Prospecting Significance in East Part of Gejiu, Yunnan. Earth Science, 36(2): 277-281. doi: 10.3799/dqkx.2011.028
    Citation: CHEN Shou-yu, ZHAO Peng-da, TONG Xiang, WU Jun-de, MO Guo-pei, CHEN Xing-shou, 2011. Metallogenic Characteristics of Western Low Altered Tin-Copper Polymetallic Deposit and Its Prospecting Significance in East Part of Gejiu, Yunnan. Earth Science, 36(2): 277-281. doi: 10.3799/dqkx.2011.028
    shu

    Metallogenic Characteristics of Western Low Altered Tin-Copper Polymetallic Deposit and Its Prospecting Significance in East Part of Gejiu, Yunnan

    doi: 10.3799/dqkx.2011.028
    • 1.

      Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

    • 2.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

    • 3.

      Yunnan Tin Company Group, Gejiu 610000, China

    • Received Date: 2010-11-30
    • Publish Date: 2011-03-01
      Abstract
    • In this paper, tin-copper polymetallic deposit in western low of east part of Gejiu is studied through a systematic analysis of its geological setting, geological characteristics of the deposit, characteristics of alterations zoning, geochemical component of altered granite, and deep exploration experience. The results show that the deposit is a part of diverse magmatic hydrothermal mineralization system, which often occurs in the inner altered granite, especially the edge and transition facies. It is a high-temperature magmatic hydrothermal deposit combining with the post-gas-liquid mineralization by the decomposition and gasification of magma in early stage and the alteration of magma intrusion in later stage. The deposit has close relationship with wall-rock alteration, especially potash feldspathization, pyritization, fluoritization and tourmalinization. The main metallic elements of the deposit include Cu, Sn, W; the elements Ag, Mo, Bi, Cd, In, U are the comprehensive utilized elements. The discovery of this type of deposits has great significance for deep exploration and further resources exploration in Gejiu mining area.

       

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      • References(10)
    • Chen, S.Y., 2009. Mineralizing multiformity and deep prospecting of Gejiu super Sn-Cu multi-metal deposit, Yunnan, China. Earth Science—Journal of China University of Geosciences, 34(2): 320-324 (in Chinese with English abstract).
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      Luo, J.L., 1995. Mineralizing pattern of Sn, W, Pb-Zn, Ag deposit, Southeast Yunnan. Yunnan Geology, 14(4): 319-332 (in Chinese).
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      Zhuang, Y.Q., Wang, R.Z., Yang, S.P., et al., 1996. Multi-metal deposit of Yunnan Gejiu. Seismological Press, Beijing, 108-124 (in Chinese).
      陈守余, 赵鹏大, 张寿庭, 等, 2009. 个旧超大型锡铜多金属矿床成矿多样性与深部找矿. 地球科学——中国地质大学学报, 34(2): 320-324. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200902015.htm
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      王新光, 朱金初, 1992. 个旧花岗岩的成因、演化及其找矿意义. 大地构造与成矿学, 16(4): 379-387. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK199204009.htm
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