Study on the Influence of Supercritical CO₂ with High Temperature and Pressure on Pore-Throat Structure and Minerals of Shale.

However, the effect of CO 2 on permeability might have an increasing trend and a possible weakening trend.

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In Figure 4 b,g, the out bound of intergranular pores showed a trend toward sphericity.

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When increasing the temperature, kaolinite, I/S mixed layer, and chlorite all exhibited a decreasing trend with increasing temperature, while the relative contents of illite increased.

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