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    Volume 43 Issue 10
    Oct.  2018
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    Li Meijun, Lai Hongfei, Mao Fengjun, Liu Jiguo, Xiao Hong, Tang Youjun, 2018. Geochemical Assessment of Source Rock within a Stratigraphic Geochemical Framework: Taking Termit Basin (Niger) as an Example. Earth Science, 43(10): 3603-3615. doi: 10.3799/dqkx.2018.223
    Citation: Li Meijun, Lai Hongfei, Mao Fengjun, Liu Jiguo, Xiao Hong, Tang Youjun, 2018. Geochemical Assessment of Source Rock within a Stratigraphic Geochemical Framework: Taking Termit Basin (Niger) as an Example. Earth Science, 43(10): 3603-3615. doi: 10.3799/dqkx.2018.223

    Geochemical Assessment of Source Rock within a Stratigraphic Geochemical Framework: Taking Termit Basin (Niger) as an Example

    doi: 10.3799/dqkx.2018.223
    • Received Date: 2018-04-02
    • Publish Date: 2018-10-20
    • How to improve the accuracy of source rock evaluation and prediction based on limited source rock samples data and geological data is a key problem that needs to be solved in the study of source rock geochemistry.By using sequence stratigraphy and petroleum organic geochemistry, this paper studies the spatial distribution and geochemical nature of source rocks of Upper Cretaceous Yogou Formation in the Termit Basin, Niger. This case study preliminarily exhibits the method, application and advantages of geochemical sequence stratigraphy. The main source beds in the Termit Basin are the marine mudstones of the Upper Cretaceous Yogou Formation, which can be divided into three third-order sequences, namely, YSQ1, YSQ2 and YSQ3 from the bottom to the top. Five types of source rocks with different sedimentary facies were subdivided on the basis of sequence/systems tracts, lithology and loggings, which include the lower offshore, upper offshore mudstones, delta and shoreface mudstones, coal seams/carbonaceous mudstones. Different sequences and systems tracts have different vertical and areal distribution patterns of these five source rock types. The organic matters from different source rocks have distinctly different geochemical characteristics. Lower and upper offshore mudstones have fair to good hydrocarbon generative potential with more contribution of lower aquatic organisms, depositing in relatively reducing environment. While delta and shoreface mudstones have good to excellent organic carbon abundances with organic matter input of both lower aquatic organisms and terrestrial organic matter, which deposited in oxidizing environment. The occurrence and lateral distribution of different types of source rocks are evidently controlled by the sedimentary facies distribution and evolution within the third-order sequences or systems tracts, and the same type of source rocks has similar geochemical characteristics. Compared with conventional source rock geochemical assessment, geochemical sequence stratigraphy can provide a practical framework to describe the detailed geochemical characteristics of different sequences, systems tracts and depositional facies within a formation or a member, and subsequently improve the accuracy of hydrocarbon resources assessment and oil-source correlation.

       

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