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    Volume 44 Issue 8
    Aug.  2019
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    Article Contents
    Wu Shijiu, Fan Caiwei, Zhao Zhanjie, Dai Long, Deng Xiaoliang, Zhong Jia, 2019. Origin of Carbonate Cement in Reservoirs of Ledong Area, Yinggehai Basin and Its Geological Significance. Earth Science, 44(8): 2686-2694. doi: 10.3799/dqkx.2019.154
    Citation: Wu Shijiu, Fan Caiwei, Zhao Zhanjie, Dai Long, Deng Xiaoliang, Zhong Jia, 2019. Origin of Carbonate Cement in Reservoirs of Ledong Area, Yinggehai Basin and Its Geological Significance. Earth Science, 44(8): 2686-2694. doi: 10.3799/dqkx.2019.154

    Origin of Carbonate Cement in Reservoirs of Ledong Area, Yinggehai Basin and Its Geological Significance

    doi: 10.3799/dqkx.2019.154
    • Received Date: 2019-02-05
    • Publish Date: 2019-08-15
    • In order to explore the distribution law, formation mechanism and its effect on reservoir quality in Ledong District, a comprehensive study of petrology and geochemistry was carried out on the characteristics of cast thin sections, carbon and oxygen isotopes, and inclusions of carbonate cement. The results show that the carbonate cement content from the slope to the depression center has been reduced from 18.0% to 5.0%, and its δ13C value is distributed in the range of -4.78‰~+1.03‰, the δ18O value is distributed in the range of -10.99‰ to -6.34‰, Z Values range from 111.27 to 123.59, ancient sea water temperature is distributed in the range of 11.36℃ to 32.02℃, ancient salinity is distributed in the range of 3.24% to 6.91%. It is found that the formation of carbonate cement is mainly related to the dissolution and precipitation of carbonate rock or high calcareous sandstone, which is controlled by the water medium temperature, the formation temperature and salinity. From the slope to the depression center, the water medium temperature is reduced, the salinity is increased, and the bond is weak. Low-content early (iron) calcite and high temperature hot fluid dissolved early (iron) calcite produced by low or high content of late (iron) dolomite areas can develop medium-permeability "sweet spot" reservoirs.

       

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