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2022 Vol. 49, No. 2
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QIN Zhengwei, FU Jianming, XING Guangfu, CHENG Shunbo, LU Youyue, ZHU Yingxue. 2022. The petrogenetic differences of the Middle-Late Jurassic W-, Sn-, Pb-Zn-Cu-bearing granites in the Nanling Range, South China[J]. Geology in China, 49(2): 518-541. doi: 10.12029/gc20220212
Citation: QIN Zhengwei, FU Jianming, XING Guangfu, CHENG Shunbo, LU Youyue, ZHU Yingxue. 2022. The petrogenetic differences of the Middle-Late Jurassic W-, Sn-, Pb-Zn-Cu-bearing granites in the Nanling Range, South China[J]. Geology in China, 49(2): 518-541. doi: 10.12029/gc20220212
shu

The petrogenetic differences of the Middle-Late Jurassic W-, Sn-, Pb-Zn-Cu-bearing granites in the Nanling Range, South China

  • 1.

    Wuhan Center of Geological Survey, China Geological Survey, Wuhan 430205, Hubei, China

  • 2.

    Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, Hubei, China

  • 3.

    Freiburg University, Freiburg 79104, Germany

  • 4.

    China University of Geosciences, Wuhan 430074, Hubei, China

    • Fund Project: Supported by NSF of China (No. 41802069)、NSF of Hubei Province (No. 2019CFB634)、China Geological Survey (No. DD20221689, No. DD20190154)
More Information
  • Author Bio: QIN Zhengwei, male, born in 1987, doctor, senior engineer, engaged in granite petrogenesis and mineralization; E-mail: qzwwto1232006@126.com
  • Corresponding author: FU Jianming, male, born in 1964, doctor, professor, engaged in petrogeochemistry; E-mail: ycfjianming@163.com 
Received Date:  08 September 2020
Revised Date:  08 March 2022
Publish Date:  25 April 2022
    Abstract

  • This paper is the result of minerial exploration engineering.

     Objective

    The Nanling Range in southern China is characterized by extensive granitic magmatic activity and significant metal deposits during the Middle-Late Jurassic, with W, Sn and Pb-Zn-Cu as the most representative metallogenic categories. In this regard, a systematic comparison study on the three types of ore-bearing granites and a thorough analysis on the origin of mineralization differences would have great implications for regional prospecting.

     Methods

    In this contribution, the whole rock major and trace element concentrations as well as geochronological, Sr-Nd-Hf isotopical and mineral chemical data of these ore-bearing granites have been collected and reviewed to summarize their petrogenetic differences.

     Results

    In combination with our major progress in the long-term geological survey, we suggest that differences do exist among W-, Sn- and Pb-Zn-Cu-bearing granites in many aspects, including the spatial-temporal distribution of the metallic deposits and related granitic plutons, geological characteristics, mineral compositions, source nature, enclave origin, differentiation degree, formation temperatures and the oxygen fugacity as well.

     Conclusions

    It is concluded that the chemical component of granitic rocks, source materials, magmatic differentiation degree and physical-chemical environment during magma evolution are closely associated with the mineralization types (W, Sn, Pb-Zn-Cu) and control the processes of ore formation. Based on the above, the integrated classification criteria for the W-, Sn- and Pb-Zn-Cu-bearing granites from the Nanling Range has been improved, which would be helpful for ore prospecting in the region.
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