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Volume 36 Issue 6
Dec 2025
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Journal of Earth Science  > 2025  >  36(6): 2387-2410.
Rui Gao, Tao Wu, Andrew C. Kerr, Han Liu, Long Xiao, Wan Huang. Zircon U-Pb Ages and Sr-Nd-Hf Isotopes Geochemistry of I-Type Granites in the Jiangda-Weixi Region, Eastern Tibet: Implications for the Tectonic Evolution of the Paleo-Tethyan Orogen. Journal of Earth Science, 2025, 36(6): 2387-2410. doi: 10.1007/s12583-024-0144-7
Citation: Rui Gao, Tao Wu, Andrew C. Kerr, Han Liu, Long Xiao, Wan Huang. Zircon U-Pb Ages and Sr-Nd-Hf Isotopes Geochemistry of I-Type Granites in the Jiangda-Weixi Region, Eastern Tibet: Implications for the Tectonic Evolution of the Paleo-Tethyan Orogen. Journal of Earth Science, 2025, 36(6): 2387-2410. doi: 10.1007/s12583-024-0144-7
shu

Zircon U-Pb Ages and Sr-Nd-Hf Isotopes Geochemistry of I-Type Granites in the Jiangda-Weixi Region, Eastern Tibet: Implications for the Tectonic Evolution of the Paleo-Tethyan Orogen

doi: 10.1007/s12583-024-0144-7
  • 1.

    College of Earth and Planetary Sciences, Chengdu University of Technology, Chengdu 610059, China

  • 2.

    Ocean College, Zhejiang University, Zhoushan 316021, China

  • 3.

    School of Earth and Environmental Sciences, Cardiff University, Cardiff CF10 3YE, UK

  • 4.

    Chengdu Center, China Geological Survey, Chengdu 610081, China

  • 5.

    School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China

  • 6.

    The 1st Geological Brigade of Hubei Province, Daye 435100, China

More Information
  • Corresponding author: Tao Wu, taowu@zju.edu.cn
  • Received Date: 20 Jun 2024
  • Accepted Date: 14 Dec 2024
  • Issue Publish Date: 30 Dec 2025
    Abstract

  • Permian–Triassic granitoids are widely distributed along the Jinshajiang suture belt, eastern Tibet, and are regarded as the result of the tectonic-magmatic activity associated with the evolution of Paleo-Tethys Ocean. This paper focuses on the high-K calc-alkaline I-type Rennong (~235 Ma) and Jiaduoling (~232 Ma) granitoid plutons, eastern Tibet, which are enriched in light rare earth elements (LREEs) and large ion lithophile elements (LILEs), but depleted in high field strength elements (HFSEs) with moderate-weak negative Eu anomalies (0.61–0.90). The Rennong granites are characterized by uniform zircon εHf(t) values (-7.3 to -3.5) and negative εNd(t) values (-7.6 to -5.7), with old two-stage Nd model ages (TDM2 = 1.51–1.46 Ga) and were likely formed by partial melting of the basement rocks, whereas the Jiaduoling rock samples have variable zircon εHf(t) values (-5.7 to +5.5) but negative εNd(t) values (-7.6 to -7.7) and are proposed to be formed by hybridization of mantle-derived mafic magma, Rennong felsic magma and sediments. Mafic microgranular enclaves (MMEs) in the Jiaduoling granitic rocks, have similar zircon U-Pb ages (~237 Ma) and zircon εHf(t) values (-4.4 to +6.3) to the host rocks, indicating that zircons in the MMEs were actually xenocrysts that formed at an early stage in the granitic magma chamber. These results reveal that the break-off of the Jinshajiang oceanic slab beneath Changdu (Qamdo)-Simao Block was in a post-collisional setting, resulted in the upwelling of asthenosphere in the Late Triassic, and then, generated the wide-spread intermediate-felsic magmatism along the Jinshajing belt, including the Rennong and Jiaduoling plutons.

     

    • Electronic Supplementary Materials: Supplementary materials (ESM I Analytical Methods and Figures S1–S3, ESM Ⅱ Tables S1–S9) are available in the online version of this article at https://doi.org/10.1007/s12583-024-0144-7.
    Conflict of Interest
    The authors declare that they have no conflict of interest.
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