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    中国百强科技报刊

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    Volume 40 Issue 5
    May  2015
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    Article Contents
    Wang Zhenfeng, Cui Yuchi, Shao Lei, Zhang Daojun, Dong Xixi, Liu Xinyu, Zhang Chuanlun, You Li, Xiao Antao, 2015. Carbonate Platform Development and Sea-Level Variations of Xisha Islands: Based on BIT Index of Well Xike-1. Earth Science, 40(5): 900-908. doi: 10.3799/dqkx.2015.074
    Citation: Wang Zhenfeng, Cui Yuchi, Shao Lei, Zhang Daojun, Dong Xixi, Liu Xinyu, Zhang Chuanlun, You Li, Xiao Antao, 2015. Carbonate Platform Development and Sea-Level Variations of Xisha Islands: Based on BIT Index of Well Xike-1. Earth Science, 40(5): 900-908. doi: 10.3799/dqkx.2015.074

    Carbonate Platform Development and Sea-Level Variations of Xisha Islands: Based on BIT Index of Well Xike-1

    doi: 10.3799/dqkx.2015.074
    • Received Date: 2014-10-25
    • Publish Date: 2015-05-15
    • In order to explore the developmental process of carbonate platform in the South China Sea (SCS) and its control factors, the organic molecular compound index method were described in this study. The branched isoprenoid tetraether (BIT) index is the ratio between the branched glycerol dialkyl glycerol tetraethers (bGDGTs) from terrigenous supply and isoprenoid GDGTs (iGDGTs) from marine crenarchaeol comprising the majority of denominator, which serves as a proxy for provenance discrimination of the organic matter and related sedimentary environments in paleoenvironmental research. The BIT curve of well Xike-1 is characterized by a unique "high-low-high" feature up section, indicating the effects of sea-level variations and carbonate platform development since Middle Miocene in the SCS. Strata with reef-beach facies were developed within carbonate platforms of Xisha Islands influenced by decrease in global as well as regional sea-level during the Late Miocene, with increased BIT values due to plenty of precipitation. Between Late Miocene and Pliocene when sea-level was higher, carbonate platforms were better formed in shallow marine environment with low BIT values. Carbonate platforms of Xisha Islands were periodically exposed in Quaternary as a result of sea-level decline over glacial cycles, leading to the second increase in BIT. Our results demonstrate that carbonate platforms of Xisha Islands have been affected by regional sea-level variations, reflecting a coupling effect on the SCS by global sea-level fluctuations and regional tectonic subductions.

       

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