Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (3): 736-753.doi: 10.13278/j.cnki.jjuese.20170058

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Mineral Chemical Characteristics and Genesis of Cassiterite in Gejiu Tin-Polymetallic Deposit, Yunnan Province

Tan Shucheng1, Guo Xiangyu1,2, He Xiaohu1, Xie Zhipeng2, Zhang Yahui1, Li Huimin3, Hao Shuang3   

  1. 1. School of Resource Environment and Earth Science, Yunnan University, Kunming 650500, China;
    2. Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China;
    3. Tianjin Center of China Geological Survey, Tianjin 300170, China
  • Received:2017-09-25 Online:2018-05-26 Published:2018-05-26
  • Supported by:
    Supported by National Natural Science Foundation of China(41262004, 41702084) and Applied Basic Research Program for Youth Project of Science and Technology Department, Yunnan Province (2017FD063)

Abstract: The Gejiu tin polymetallic deposit is located in the west of the southeastern Yunnan tin ore belt, and is one of the largest tin polymetallic deposits in the world. As the main ore minerals in the Gejiu tin-polymetallic deposit,the mineral chemical characteristics of cassiterite have a great implication to the ore genesis. In this research, we studied the internal structure and the mineral chemical characteristics of cassiterites out of six types of ores in the Gejiu tin-polymetallic using the scanning electron microscopy and electron probe microscope analyzer. The results of scanning electron microscopy show that except the interlayer oxidation broken ore type cassiterites,the zonal structure is clearly developed within cassiterites. The results of electron probe microscope analyzer (EPMA) show that the variation range of the mass fraction of SnO2 is 97.700%-101.728%, and the mass fractions of Ta2O5, FeO, ZrO2 and HfO2 are high, which indicates that these cassiterites may be precipitated in a high temperature environment. The value of (Fe+Mn)/(Nb+Ta) shows that the different types of cassiterites have the characteristics of hydrothermal cassiterites. Very low mass fractions of Nb2O5 and MnO in different types of cassiterites suggest that the ore-forming fluid may be derived from the high-fractionated granitic magma. The mass fractions of Na, Ta indicate that the mineralization occurred in an acid to weak acid environment. The gradually decreased In2O3 in different ores (including sulfide, skarn, tourmaline veinlet belt, tin-bearing dolomite, and interlayer oxidation types of ores) indicates that the ore forming temperature and pressure have decreased gradually. However, the average mass fractions of In2O3 in greisen type need further study. The change of the physicochemical conditions of magma hydrothermal fluid during the formation of cassiterite resulted in the formation of its internal zonal structure. The electron probe data shows that the chemical composition in the zonal structure of cassiterite is "serrated", indicating that the mineralization occurred in turbulence, so the cassiterite deposits have multi-stage characteristics.

Key words: mineral chemistry, electron probe microscope analyzer, cassiterite, Gejiu tin-polymetallic deposit

CLC Number: 

  • P618.4
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