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    中国百强科技报刊

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    Volume 39 Issue 9
    Sep.  2014
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    Article Contents
    Li Min, Han Zongzhu, Xu Hong, Zhao Guangtao, Zhang He, Lai Zhiqing, 2014. Metamorphic P-T-t Path of Eclogites from Qianliyan Island in the South Yellow Sea and Its Tectonic Implications. Earth Science, 39(9): 1289-1300. doi: 10.3799/dqkx.2014.110
    Citation: Li Min, Han Zongzhu, Xu Hong, Zhao Guangtao, Zhang He, Lai Zhiqing, 2014. Metamorphic P-T-t Path of Eclogites from Qianliyan Island in the South Yellow Sea and Its Tectonic Implications. Earth Science, 39(9): 1289-1300. doi: 10.3799/dqkx.2014.110

    Metamorphic P-T-t Path of Eclogites from Qianliyan Island in the South Yellow Sea and Its Tectonic Implications

    doi: 10.3799/dqkx.2014.110
    • Received Date: 2014-01-08
    • Publish Date: 2014-09-01
    • The eclogites in Qianliyan Island, the South Yellow Sea, is important for conducting further research of Dabie-Sulu Orogen. Petrographic and mineralogic studies reveal four main metamorphic stages, including prograde (Stage Ⅰ), eclogite-facies (Stage Ⅱ) metamorphism, and amphibolite-(Stage Ⅲ), greenschist-facies (Stage Ⅳ) retrograde metamorphisms. The metamorphic P-T conditions are estimated as follows: Stage Ⅱ, T=806.3 ℃, P=3.32 GPa; Stage Ⅲ, T=658.68 ℃, P=0.78 GPa; Stage Ⅳ, T < 550 ℃, P < 0.3 GPa. The SHRIMP U-Pb datings of the zircons from eclogites show that the protoliths were formed in Neoproterozoic (about 747±19 Ma), the UHP metamorphism happened in Early Triassic (about 241.1±1.5 Ma), and the amphibolite-facies retrograde metamorphism happened in the end of Triassic (about 205.8 Ma). Using the data mentioned above, metamorphic PTt path of eclogites is constructed. The PTt path shows that the eclogites experienced 2 stages of exhumation and reveals that the Qianliyan uplift is the extension of Sulu Orogen in the South Yellow Sea.

       

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