Water is easily preserved in the pores and forms the undercompaction of the mudstone layer.

具欠压实地层的孔隙水承担了部分上覆地层的重量，从而形成孔隙流体超压。

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Water is easily preserved in the pores and forms the undercompaction of the mudstone layer.

具欠压实地层的孔隙水承担了部分上覆地层的重量，从而形成孔隙流体超压。

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