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    Volume 41 Issue 5
    May  2016
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    Ding Xiujian, Liu Guangdi, Huang Zhilong, Lu Xuejun, Chen Zhelong, Gu Feng, 2016. Ding Xiujian, Liu Guangdi, Huang Zhilong, Lu Xuejun, Chen Zhelong, Gu Feng. Earth Science, 41(5): 832-842. doi: 10.3799/dqkx.2016.070
    Citation: Ding Xiujian, Liu Guangdi, Huang Zhilong, Lu Xuejun, Chen Zhelong, Gu Feng, 2016. Ding Xiujian, Liu Guangdi, Huang Zhilong, Lu Xuejun, Chen Zhelong, Gu Feng. Earth Science, 41(5): 832-842. doi: 10.3799/dqkx.2016.070

    Ding Xiujian, Liu Guangdi, Huang Zhilong, Lu Xuejun, Chen Zhelong, Gu Feng

    doi: 10.3799/dqkx.2016.070
    • Received Date: 2015-08-25
    • Publish Date: 2016-05-15
    • The debate on formation of source rocks has been focused on "productivity mode" and "preservation mode" in marine sediments for many years. Based on the datasets of total organic carbon, carbonate carbon isotope, pyrolysis parameters and reduced sulfur of source rocks of Erlian basin, the productivity and terrigenous organic matter input are characterized and then the role of organic matter supply and preservation in the formation of source rocks are discussed. For the lacustrine basin with high organic matter supply, organic matter supply is the main factor controlling the formation on source rocks because there are still source rocks formed by accumulation of residual organic matter even in the oxidizing sedimentary environment. For the lacustrine basin with low organic matter supply, preservation is the main factor controlling the formation on source rocks because the organic matter can only be preserved in reducing environment since it is too rare to be preserved from oxidation.

       

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