Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (3): 749-766.doi: 10.13278/j.cnki.jjuese.20200117

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Geochronology, Geochemical Characteristics and Genesis of Napeng Granite Biotite Monzogranite in Yunkai Area, Guangxi

Tian Mengyu, Di Yongjun, Wang Shuai, Jia Yilong   

  1. School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China
  • Received:2020-05-08 Online:2021-05-26 Published:2021-06-07
  • Supported by:
    Supported by the Project of China Geological Survey (DD20190379-79) and China Geological Survey Research Contract ([2018]No.62,[2019]No.106)

Abstract: The Indosinian period in South China experienced intense tectonic movement and magmatic activity, and the tectonic background of the Indosinian granite has always been a hot topic in earth science. A detailed study was conducted on the chronology, geochemical characteristics and genesis of zircon of the biotite monzogranite of Napeng in Yunkai area, Guangxi. The results show that the weighted average age of zircon U-Pb LA-ICP-MS zircon is (257.8 ±1.2) Ma, and the chemical analyses show that the Late Permian granitoids are classified as alkali-calcic rocks, which are characterized by enrichment of light rare earth elements (LREEs), large ion lithophile elements (LILEs), depletion of heavy rare earth elements (HREEs) and high field strength elements (HFSEs), and Ba, Sr, and obvious negative europium anomaly(δEu=0.41-0.66). All the geochemical characteristics suggest that the Napeng granitoid pluton experienced highly differentiated evolution. Through analyses, the material source of granite may come from the partial melting of the mixed sand-muddy source rocks in the ancient crust, and the tectonic environment may be formed in the post-mountain stage of the plate collision junction environment.

Key words: geochronology, geochemistry, biotite monzogranite, Yunkai area, Guangxi

CLC Number: 

  • P588.12
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