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2023 Vol. 50, No. 5
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OUYANG Junyong, ZHANG Shuming, ZHANG Xin, LIU Long, XIA Yinchu, WU Zhichun, WAN Kang. 2023. Magmatic evolution characteristics of two types of rhyolite dacite in Xiangshan uranium ore field——Evidence from chemical composition of feldspar and biotite[J]. Geology in China, 50(5): 1495-1512. doi: 10.12029/gc20201110002
Citation: OUYANG Junyong, ZHANG Shuming, ZHANG Xin, LIU Long, XIA Yinchu, WU Zhichun, WAN Kang. 2023. Magmatic evolution characteristics of two types of rhyolite dacite in Xiangshan uranium ore field——Evidence from chemical composition of feldspar and biotite[J]. Geology in China, 50(5): 1495-1512. doi: 10.12029/gc20201110002
shu

Magmatic evolution characteristics of two types of rhyolite dacite in Xiangshan uranium ore field——Evidence from chemical composition of feldspar and biotite

  • 1.

    State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang, 330013, Jiangxi, China

  • 2.

    Hunan Geosun Hi-technology Co., Ltd., Changsha 410006, Hunan, China

  • 3.

    Key Laboratory of Radioactive Geology and Exploration Technology FundamentalScience for National Defense, East China University of Technology, Nanchang 330013, Jiangxi, China

  • 4.

    Gandong University, Fuzhou 344000, Jiangxi, China

    • Fund Project: Supported by projects of National Natural Science Foundation of China (No.41862006, No.41802247) and Postgraduate Student Innovation Special Fund Project in Jiangxi Province (No.YC2020-B159)
More Information
  • Author Bio: OUYANG Junyong, male, born in 1993, master candidate, majors in geology; E-mail: 3423328173@qq.com
  • Corresponding author: ZHANG Shuming, male, born in 1965, professor, mainly engaged in research of uranium geology and teaching of basic geology; E-mail: shmzhang@ecut.edu.cn 
Received Date:  10 November 2020
Revised Date:  13 January 2021
Publish Date:  25 October 2023
    Abstract

  • This paper is the result of mineral exploration engineering.

     Objective

    Minerals formed by magmatic differentiation, such as feldspar and biotite, can be used as indicators of magmatic evolution of host rocks.There are disputes between rhyodacite and rhyodacite porphyry from Xiangshan, in the aspects of formation age, origin, material source and mantle material participation.

     Methods

    In this paper, the electron probe technology is used to quantitatively analyze the feldspar and biotite in two types of rhyodacites in Xiangshan, and the composition, material source, formation temperature, oxygen fugacity and rock properties of the two types of rhyodacites are analyzed and studied.

     Results

    The results show that the rhyodacite of Xiangshan Daguding Formation can be divided into two types, one is the effusive rhyodacite (K1d2a) and the other is the intrusive rhyodacite porphyry (K1d2b). The types of feldspar from rhyodacite are more than those of rhyodacite porphyry. The feldspar types of rhyodacite include albite, potassium feldspar, potassium sanidine, feldspar and andesine. The main feldspar types of rhyodacite porphyry are albite, potassium feldspar and potassium-sanidine. The biotite formation temperature of rhyodacite and rhyodacite porphyry is basically the same (750±20℃). Rhyodacite and rhyodacite porphyry both have high oxygen fugacity and belong to calc-alkaline rocks, indicating the same magma material source with part from mantle material.

     Conclusions

    The chemical composition is basically the same, together with the same feldspar type, the same material source, the same crystallization temperature, the sameoxygen fugacity, and the same rock properties, indicating that the two have homology.
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