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    中国百强科技报刊

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    Volume 45 Issue 6
    Jun.  2020
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    Article Contents
    Han Qingsen, Peng Songbai, Jiao Shujuan, 2020. Discovery and Tectonic Implications of Paleoproterozoic Cold Subduction Low-Temperature/High-Pressure Eclogitic Metapelites, Yangtze Craton. Earth Science, 45(6): 1986-1998. doi: 10.3799/dqkx.2020.074
    Citation: Han Qingsen, Peng Songbai, Jiao Shujuan, 2020. Discovery and Tectonic Implications of Paleoproterozoic Cold Subduction Low-Temperature/High-Pressure Eclogitic Metapelites, Yangtze Craton. Earth Science, 45(6): 1986-1998. doi: 10.3799/dqkx.2020.074

    Discovery and Tectonic Implications of Paleoproterozoic Cold Subduction Low-Temperature/High-Pressure Eclogitic Metapelites, Yangtze Craton

    doi: 10.3799/dqkx.2020.074
    • Received Date: 2020-01-11
    • Publish Date: 2020-06-15
    • In this paper, it documents for the first time the presence of the distinctive Grt-Ky-Cld assemblage low-temperature/high-pressure (LT-HP) eclogitic metapelites from the Paleoproterozoic Shuiyuesi mélange belt in the Kongling complex, Yangtze craton. The high-pressure metapelites display peak metamorphic mineral assemblages of garnet+kyanite+chloritoid+phengite+rutile+quartz. A near-isothermal decompression (ITD) clockwise P-T path with peak conditions of 571-576 ℃ and 19.2-21.8 kbar were estimated by phase equilibria modelling. The LA-ICP-MS zircon U-Pb dating shows that the metapelite has a metamorphic age of 1 991±20 Ma recorded by zircon rims and ages ranges from 2.1 to 2.2 Ga recorded detrital zircon cores. The sedimentary tectonic setting and metamorphic peak conditions of the Grt-Ky-Cld assemblage in eclogitic metapelites indicate that it has formed in a cold subduction zone with low thermal gradient (dT/dP≈300 ℃/GPa) at the active continental margin. Our study further implies that the modern plate tectonics with "cold subduction" tectonic characteristics has been initiated at least since the Paleoproterozoic.

       

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