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Volume 36 Issue 6
Dec 2025
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San Win, Qinglai Feng, Ye Myint Swe, Tianyu Zhao, Zhengqin Gan, Xiaomei Nie, Aung Khaing, Sai Naing Lin Aung. Early Carboniferous Magmatic Rocks in Eastern Myanmar: Implications for the Tethyan Evolution. Journal of Earth Science, 2025, 36(6): 2450-2464. doi: 10.1007/s12583-022-1723-0
Citation: San Win, Qinglai Feng, Ye Myint Swe, Tianyu Zhao, Zhengqin Gan, Xiaomei Nie, Aung Khaing, Sai Naing Lin Aung. Early Carboniferous Magmatic Rocks in Eastern Myanmar: Implications for the Tethyan Evolution. Journal of Earth Science, 2025, 36(6): 2450-2464. doi: 10.1007/s12583-022-1723-0

Early Carboniferous Magmatic Rocks in Eastern Myanmar: Implications for the Tethyan Evolution

doi: 10.1007/s12583-022-1723-0
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  • Corresponding author: Qinglai Feng, qinglaifeng@cug.edu.cn
  • Received Date: 20 Apr 2022
  • Accepted Date: 22 Jul 2022
  • Issue Publish Date: 30 Dec 2025
  • Eastern Myanmar is the key position linking between SW Yunnan and northern Thailand for better understanding of Tethyan evolution. However, the actual location and evolution of the Tethyan suture zone are still unclear in eastern Myanmar. The present study focuses on the geochronological, geochemical and zircon Lu-Hf isotopic study on the plutonic rocks, including granite, diorite and gabbroic rocks, from the Tachileik area, eastern Myanmar. These plutonic rocks yielded zircon U-Pb weighted mean ages of ca. 353–355 Ma, suggesting the Early Carboniferous emplacement. The Tachileik granites are high-K calc-alkaline, weakly peraluminous and have low P2O5 contents, which are typical features of Ⅰ-type granites. They have positive zircon εHf(t) values (+4.5– +7.4) with TDM2 ages of 981–825 Ma, indicating a juvenile mafic lower crust source. The Tachileik gabbros and diorites show high Al2O3 contents and Mg#, but low TiO2 and K2O contents, belonging to tholeiitic and calc-alkaline basalt series. They are characterized by enrichments in large ion lithophile elements (LILEs, e.g., Rb, Ba and Sr), depletions in high field strength elements (HFSEs) and distinctly negative Nb and Ta anomalies, similar to the volcanic arc basalt. The zircon Hf isotopic (+4.7– +7.1) and whole-rock geochemical data imply that the Tachileik gabros and diorites probably resulted from partial melting of lithospheric mantle in the spinel stability field within an arc-related setting. The magmatic rocks can be grouped to the Late Devonian–Early Carboniferous magmatic rock and pyroclastic rock zone from SW Yunnan to northern Thailand based on their age and geochemical characters. The zone was formed in the post-collisional extension-related tectonic setting of the Proto-Tethys. This study provides important evidences for the evolution of the Proto-Tethys in Southwest Yunnan and Southeast Asia.

     

  • Electronic Supplementary Materials: Supplementary materials (Tables S1–S3) are available in the online version of this article at https://doi.org/10.1007/s12583-022-1723-0.
    Conflict of Interest
    The authors declare that they have no conflict of interest.
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