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    Volume 39 Issue 5
    May  2014
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    Article Navigation >  Earth Science  > 2014  >  39(5): 509-524
    Zhang Shuo, Shi Hongfeng, Hao Haijian, Li Dewei, Lin Yan, Feng Minxuan, 2014. Geochronology, Geochemistry and Tectonic Significance of Late Cretaceous Adakites in Bangong Lake, Tibet. Earth Science, 39(5): 509-524. doi: 10.3799/dqkx.2014.049
    Citation: Zhang Shuo, Shi Hongfeng, Hao Haijian, Li Dewei, Lin Yan, Feng Minxuan, 2014. Geochronology, Geochemistry and Tectonic Significance of Late Cretaceous Adakites in Bangong Lake, Tibet. Earth Science, 39(5): 509-524. doi: 10.3799/dqkx.2014.049
    shu

    Geochronology, Geochemistry and Tectonic Significance of Late Cretaceous Adakites in Bangong Lake, Tibet

    doi: 10.3799/dqkx.2014.049
    • 1.

      Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China

    • 2.

      Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • 3.

      Research Center for Tibetan Plateau, China University of Geosciences, Wuhan 430074, China

    • 4.

      Nanjing Center, China Geological Survey, Nanjing 210000, China

    • 5.

      Shaanxi Nuclear Industry Geology Surveying Institute, Xi'an 710000, China

    • Received Date: 2013-08-19
    • Publish Date: 2014-05-01
      Abstract
    • Risong rocks and Jiawei acid rock veins are located at Bangong Lake ophiolite mélange belt, western Tibetan Plateau. The lithology is tonalite, corcovadite and granodiorite, displaying a transition from medium-K calc-alkaline series to high-K calc-alkaline series. Rocks show geochemical characteristics of adakites, having high content of SiO2 (63.05%~70.72%), Al2O3(≥15%), Sr (380.4×10-6-625.0×10-6), Sr/Y ratio(> 35) and low content of MgO (0.97%-2.33%) < 3%, HREE, Y(5.64×10-6-13.80×10-6) and Yb(0.46×10-6-1.25×10-6). The differentiation is obvious between HREE and LREE (17.09 < (La/Yb)N < 48.51). Risong granodiorite is dated to 82.0±1.1 Ma by zircon U-Pb dating method; east-west trend granodiorite and south-north trend corcovadite are dated to 90.7±1.2 Ma, 82.9±1.2 Ma respectively. Risong and Jiawei adakitic rocks are enriched in K and depleted in Na, and have low Cr, Ni, Sr/Y and high Th, Th/La, Th/U, Rb/Sr and Mg#(43.09-54.35). These characteristics indicate that they were formed by partial melting of thickened lower crust which was caused by basaltic magma underplating. 91-82 Ma adakites were formed in the early stage after the collision as the product of both interplates thermal upwelling extension and crust-mantle interaction after the closure of Meso-Tethys. Outcropping of adakites in this period can mark the transition from the plate tectonic system to intraplate tectonic system.

       

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