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2023 Vol. 50, No. 2
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TAO Qin, HAN Runsheng, ZHAO Dong, WU Peng, TIAN Xufeng, ZHAO Taicheng, YANG Hang, ZONG Zhihong, DENG Anping. 2023. The mineralization and alteration zoning model related to the concealed granite porphyry of the Huangshaping Cu-Sn polymetallic deposit, Southern Hunan Province[J]. Geology in China, 50(2): 586-604. doi: 10.12029/gc20191211003
Citation: TAO Qin, HAN Runsheng, ZHAO Dong, WU Peng, TIAN Xufeng, ZHAO Taicheng, YANG Hang, ZONG Zhihong, DENG Anping. 2023. The mineralization and alteration zoning model related to the concealed granite porphyry of the Huangshaping Cu-Sn polymetallic deposit, Southern Hunan Province[J]. Geology in China, 50(2): 586-604. doi: 10.12029/gc20191211003
shu

The mineralization and alteration zoning model related to the concealed granite porphyry of the Huangshaping Cu-Sn polymetallic deposit, Southern Hunan Province

  • 1.

    Kunming University of Science and Technology, College of Land and Resources Engineering, Kunming 650093, Yunnan, China

  • 2.

    Southwest Institute of Geological Survey, Geological Survey Center for Non-ferrous Mineral Resources, Kunming 650093, Yunnan, China

  • 3.

    Southern Hunan Institute of Geology Survey, Chenzhou 423000, Hunan, China

  • 4.

    Hunan Nonferrous Huangshaping Mining Co. Ltd, Chenzhou 424421, Hunan, China

    • Fund Project: Supported by National Key Research and Development Program (No.2018YFC0603902), the projects of Yunling Scholars (2014), Yunnan engineering laboratory of mineral resources prediction and evaluation (2010), and geological process and mineral resources innovation team (2012)
More Information
  • Author Bio: TAO Qin, female, born in 1993, master, majors in mineralogy, petrology, mineral deposit geology; E-mail: 894474134@qq.com
  • Corresponding author: HAN Runsheng, male, born in 1964, professor, supervisor of doctor candidates, engaged in the dynamics of tectonic ore-forming processes and prognosis of concealed deposit; E-mail: 554670042@qq.com 
Received Date:  11 December 2019
Revised Date:  08 April 2020
Publish Date:  25 April 2023
    Abstract

  • This paper is the result of mineral exploration engineering.

     Objective

    The Huangshaping Cu-Sn polymetallic deposit is one of the typical representatives of the magmatic hydrothermal metallogenic system in southern Hunan, China. In order to deepen the diagenetic and metallogenic mechanism of the deposit and efficiently guide the exploration of deep prospecting, it is necessary to reveal the polymetallic mineralization-alteration zone rule related to the concealed granite porphyry, and construct the deep mineralization-alteration spatial zoning model.

     Methods

    Applying the large-scale altered lithofacies location prospecting and prediction method for hydrothermal deposits, and the geochemical analysis of rock and mineral for tunnel sections in the typical levels of -136 m, -176 m and -256 m, the intensity change of mineralization-alteration, mineral paragenetic association and its spatial zoning characteristics were analyzed, and the transformation rules of ore-forming elements, element associations and element ratios were discussed.

     Results

    The current study constructed mineralization-alteration zoning model: from porphyry (internal zone) to contact zone to surrounding rock (outer zone) with scheelite-molybdenite (pyrite) mineralized-silicified-sericitized granite porphyry zone (Ⅰ) → magnetization (scheelite-cassiterite) mineralized garnet skarn zone (Ⅱ-1) → scheelite-molybdenite-pyrrhotite mineralized garnet skarn zone (Ⅱ-2) → lead-zinc mineralized crystalline limestone zone (Ⅲ) → strong calcitization limestone zone (Ⅳ). The main mineral assemblages of in the corresponding zones are: Quartz + (Pyrite + Sericite) → Magnetite + Diopside + Wollastonite + Epidote + Chlorite + (Scheelite + Cassiterite + Pyrite + Garnet) → Scheelite + Molybdenite + Pyrrhotite + (Cassiterite + Chalcopyrite + Pyrite + Sphalerite + Galena) + Garnet + Vesuvianite + Diopside + Hornblende + Fluorite + Epidote + Chlorite + (Quartz + Calcite) → Galena + Sphalerite + (Pyrite) + Calcite + Quartz → Calcite + Quartz. The distribution rule of mineralized elements in each alteration zone was revealed: W, Mo → Fe, W, Sn (Bi, Mo) → W, Sn, Bi, Mo (Cu) → Pb, Zn (W, Sn, Cu) → Pb, Zn, Ag.

     Conclusions

    The mineralization-alteration zoning rule of the deposit was obvious from the rock mass as the center to the surrounding rock on both sides. The transformation rules of characteristic mineral assemblage and mineralization indicator elements in each zone have an obvious indication of the occurrence position of the ore body.
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