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2024 Vol. 45, No. 4
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WANG Jiasheng, FU Hao, HOU Defa, WANG Yongrui, LI Haiming, ZHAO Jianhua. 2024. The “Two-story Binary Metallogenic Model” for Pure Stibnite Deposits in the South China Antimony Ore Belt: A Case Study of the Muli Antimony Deposit in Southeastern Yunnan Province. Acta Geoscientica Sinica, 45(4): 502-514. doi: 10.3975/cagsb.2024.022601
Citation: WANG Jiasheng, FU Hao, HOU Defa, WANG Yongrui, LI Haiming, ZHAO Jianhua. 2024. The “Two-story Binary Metallogenic Model” for Pure Stibnite Deposits in the South China Antimony Ore Belt: A Case Study of the Muli Antimony Deposit in Southeastern Yunnan Province. Acta Geoscientica Sinica, 45(4): 502-514. doi: 10.3975/cagsb.2024.022601
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The “Two-story Binary Metallogenic Model” for Pure Stibnite Deposits in the South China Antimony Ore Belt: A Case Study of the Muli Antimony Deposit in Southeastern Yunnan Province

  • 1. Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming, Yunnan 650093;

  • 2. 149th Team, Gansu Coal Geology Bureau, Lanzhou, Gansu 730020;

  • 3. Yunnan Muli Antimony Industry Co., Ltd., Wenshan, Yunnan 663099

Received Date:  12 October 2023
Revised Date:  06 February 2024
    Abstract
  • The South China antimony ore belt, which is composed of lots of large-super large pure stibnite deposits, is the most important antimony metallogenic belt in China and even in the world.In this study, the Muli antimony deposit in southeastern Yunnan province, was taken as a main research object, through the detailed comparative study of basic geological characteristics with the typical Xikuangshan and Dushan antimony ore fields (deposits) in the South China antimony ore belt.We can find that no matter in ore field or deposit scale for the pure stibnite ore field (deposit), two types of ore may occur, “quartz-stibnite” and “calcite-stibnite”.In the same ore field, some deposits (sections) show “quartz-stibnite” mineral assemblage, while some show“calcite-stibnite” mineral assemblage.On the other hand, the “quartz-stibnite” mineral assemblage usually located in the upper part, and “calcite-stibnite” mineral assemblage located in the lower part when they contemporaneously exist in one deposit.Such model is first named as “two-story binary metallogenic model” in this paper, which is of great significance for the study of genesis and prospecting of pure stibnite deposits in South China antimony ore belt.
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