Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (4): 1119-1138.doi: 10.13278/j.cnki.jjuese.20200131

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Permian Volcanic Rocks in Kalatage Area, Eastern Tianshan, Xinjiang: Petrogenesis and Tectonic Implications

Zhang Xue1, Weng Kai2, Zhao Xiaojian2, Du Shouli3, Shang Ying4   

  1. 1. School of Earth Science and Resources, Chang'an University, Xi'an 710054, China;
    2. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR/Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China;
    3. Research Institute of Exploration and Development, Changqing Oilfield Company, PetroChina, Xi'an 710018, China;
    4. National Research Center for Geoanalysis, Chinese Academy of Geological Sciences, Beijing 100037, China
  • Received:2020-06-01 Online:2021-07-26 Published:2021-08-02
  • Supported by:
    Supported by the Projects of Fundamental Research Funds of the Central Universities for Chang'an University (300102270110), the Natural Science Foundations of Shannxi Province,China (2021JQ-329,2020JQ-440) and the National Natural Science Foundation of China (41602236)

Abstract: The Kalatage area is located in the north central part of the Eastern Tianshan, where the Permian continental volcanic rocks are widely distributed. Their petrography, geochemistry, zircon U-Pb geochronology,and Lu-Hf isotope analysis for basalt and dacite are presented in this paper. The LA-ICP-MS zircon U-Pb dating of (267.5±1.5) Ma and (296.7±1.7) Ma from two dacite samples represents the crystallization age of dacite in the Early Permian. The geochemical data show that the basalt is of alkaline series with high Al2O3,Na2O/K2O, low TFeO, Mg#, and Cr. The Ta, La, and Nb contents standardized by Yb indicate its basaltic magmatic origin from the enriched mantle source. The low La/Ba, (Th/Nb)N>1 and Nb/La<1 suggest that the magma was mixed with lithospheric material during its ascent. The samples have w(Zr)>100×10-6 and Zr/Y>5, indicating the characteristics of continental intraplate basalt. The dacite is of calc-alkaline type with enrichment of silicon and aluminum, high contents of Rb, Ba, Th, U, Zr, etc, and low content of Ti, Nb, Ta, Sr, P, etc. These features are obviously different from those of the basalt but similar to the crust. The dacite has positive εHf(t) value (5.4-14.7), indicating that the source region is the new crust. The w(Y+Nb)-w(Rb) discrimination diagrams of tectonic setting show that the dacite was formed in the continental extensional setting. Combined with the previous research results, we believe that the Kalatage Early Permian volcanic rocks formed in the continental extensional setting, and they are part of the Carboniferous-Permian rift-related volcanism in Tianshan, which restricted the closure of Paleo-Asian Ocean in this area before the Early Permian.

Key words: Eastern Tianshan, Permian, volcanic rocks, zircon U-Pb dating, geochemistry, petrogenesis

CLC Number: 

  • P581
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