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    中国百强科技报刊

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    Volume 37 Issue 4
    Jul.  2012
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    Article Contents
    LEI Zhen-yu, XIE Xi-nong, MENG Yuan-lin, HUANG Wei, DU Xue-bin, XIAO Li-hua, MENG Fan-jin, JIAO Jin-he, LIU Wen-hui, 2012. Effecting of Overpressures on Diagensis in the Qijiagulong-Sanzhao Depression of Songliao Basin. Earth Science, 37(4): 833-842. doi: 10.3799/dqkx.2012.092
    Citation: LEI Zhen-yu, XIE Xi-nong, MENG Yuan-lin, HUANG Wei, DU Xue-bin, XIAO Li-hua, MENG Fan-jin, JIAO Jin-he, LIU Wen-hui, 2012. Effecting of Overpressures on Diagensis in the Qijiagulong-Sanzhao Depression of Songliao Basin. Earth Science, 37(4): 833-842. doi: 10.3799/dqkx.2012.092

    Effecting of Overpressures on Diagensis in the Qijiagulong-Sanzhao Depression of Songliao Basin

    doi: 10.3799/dqkx.2012.092
    • Received Date: 2012-02-28
      Available Online: 2021-10-13
    • Publish Date: 2012-07-15
    • There are 3 sets of obvious overpressure systems in the strata above the Qingshankou Formation in Qijiagulong-Sanzhao depression, Songliao basin. The overpressure in the Qingshankou (K2qn) and Nenjiang (K2n) Formation mud rock which is the key zone of exploration which not only controls the formation of hydrocarbon, but also impacts the adjacent reservoir property deeply. Based on the previous studies, this paper utilizes abundant materials, including thermal decomposition, X-ray diffraction, microscope analysis, SEM and blue epoxy resin-impregnated thin sections, to study the effect of overpressure on diagenesis. The results indicate: (1) the overpressure constrained the transformation of clay minerals, and also depressed the evolution of hydrocarbon structure. (2) The compaction and cementation during diagenesis responded apparently to the overpressure depression. The overpressure didn't affects dissolution directly, but via the geo-fluids indirectly, causing the increase of porosity by induced pore.

       

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