Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (3): 842-856.doi: 10.13278/j.cnki.jjuese.20180316

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Mineral Compositional and Chronological Characteristics of Guposhan Pluton in Guangxi and Its Petrogenetic and Metallogenic Significance

Cai Yongfeng1,2, Liu Fenglei1, Feng Zuohai1,2, Zhou Yun1, Zeng Changyu3   

  1. 1. Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, Guilin University of Technology, Guilin 541004, Guangxi, China;
    2. Collaborative Innovation Center for Exploration of Hidden Nonferrous Metal Deposits and Development of New Materials in Guangxi, Guilin University of Technology, Guilin 541004, Guangxi, China;
    3. Guangxi Geological Survey Institute, Nanning 530023, China
  • Received:2018-12-01 Published:2020-05-29
  • Supported by:
    Supported by Guangxi Natural Science Foundation Program (2018GXNSFBA281069, 2015GXNSFDA139029, 2017GXNSFAA198209), Key Programs of Higher Education of Guangxi Autonomous Region (KY2015ZD052) and the Fifth Bagui Scholar Innovation Project of Guangxi Autonomous Region (2018,Metallogenic Theory and Exploration Technique of Nonfreus Metals)

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Abstract: In order to reveal the distribution of Early Yanshanian magmatism and its petrogenetic and metallogenic significance in South China,the authors studied the mineral composition and LA-ICP-MS zircon U-Pb geochronological characteristics of Guposhan pluton, which intruded in Huashan-Guposhan belt in northeast Guangxi. The geochronological analyses show two crystallized ages of (162±3) and (163±2) Ma, which are consistent with the time of Mesozoic large scale magmatism and mineralization in South China. The result of electron microprobe analyzer (EMPA) suggests that the biotite from Guposhan pluton has high TFeO and low MgO contents with Fe/(Fe+Mg) values of 0.68-0.84, resembling those of siderophyllite. The negative correlation between TFeO and MgO shows that the replacement between Fe2+ and Mg2+ occurred during crystallization of biotite. The data of biotite thermometers show high crystallization temperature of 680-705℃ and low oxygen fugacity of -17.0--15.5. The results of Al-in-biotite barometer indicate the biotite crystallization pressure is 69-179 MPa, suggesting a crystallization depth of 2 621-6 755 m. Integrated with regional geological data, it could be inferred that the Early Yanshanian (~162 Ma) granitic magmatism is a common geological process, and a large scale of lithospheric extension and thinning might be the key mechanism to drive the Mesozoic magmatism and the corresponding mineralization in South China. Relatively high temperature, low oxygen fugacity, and shallow environment are favorable for Sn mineralization.

Key words: granite, biotite, zircon U-Pb geochronology, Guposhan pluton, northeast Guangxi

CLC Number: 

  • P588.1
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