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    Volume 45 Issue 5
    May  2020
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    Article Navigation >  Earth Science  > 2020  >  45(5): 1556-1572
    Li Chengzhi, Yang Wenguang, Zhu Lidong, Lin Limin, Su Xin, Zhang Hongliang, 2020. Geochemistry, Petrogenesis and Geological Significance of Early Jurassic Granite in Mozhugongka Area, Tibet. Earth Science, 45(5): 1556-1572. doi: 10.3799/dqkx.2019.196
    Citation: Li Chengzhi, Yang Wenguang, Zhu Lidong, Lin Limin, Su Xin, Zhang Hongliang, 2020. Geochemistry, Petrogenesis and Geological Significance of Early Jurassic Granite in Mozhugongka Area, Tibet. Earth Science, 45(5): 1556-1572. doi: 10.3799/dqkx.2019.196
    shu

    Geochemistry, Petrogenesis and Geological Significance of Early Jurassic Granite in Mozhugongka Area, Tibet

    doi: 10.3799/dqkx.2019.196
    • 1.

      School of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China

    • 2.

      Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

    • Received Date: 2019-08-06
    • Publish Date: 2020-05-15
      Abstract
    • In order to explore the petrogenesis types and tectonic setting of the Late Triassic-Early Jurassic magmatic rocks in the southern Gangdese, we report detailed petrography, geochronology, and whole-rock geochemistry of the Songduo biotite monzogranite plutons in the Mozhugongka area.The zircon LA-ICP-MS U-Pb dating results show that the age of the Songduo biotite monzogranite plutons is 190.2±2.9 Ma, indicating that it was formed in the Early Jurassic.In terms of geochemical composition, the Songduo biotite monzogranite plutons have low TiO2 (0.68%-0.75%), high SiO2 (65.22%-66.13%), Al2O3 (16.26%-16.73%), Na2O (4.05%-4.29%), and K2O (3.96%-4.24%) contents, belonging to the shoshonite series and weakly-peraluminous (A/CNK=1.04-1.11);In the spidergram, the samples show enrichment in Rb, Th, K, Zr and Hf, and depletion in Ba, Nb, Ta, Sr, Ti and P. The whole-rock zircon saturation temperature varies from 805 to 835 ℃, with high FeOT/MgO ratios. The Songduo pluton has an affinity with A-type granite. In combination with pervious research results, it shows that the Late Triassic-Early Jurassic magmatic rocks in central and southern Gangdese were formed in magmatic arc related to the northward subduction of the Neo-Tethys oceanic slab. We suggest that the Songduo biotite monzogranite plutons generated in a back-arc extensional environment during the subduction of the Neo-Tethys oceanic slab, and the formation of granite is related to the partial melting of the lower crust caused by the intrusion of mantle-derived magma.

       

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