低渗透性的沉积物在快速沉降过程中 ,上覆岩层产生的不均衡压实可产生相当大的超压 ,这是沉积盆地形成高压的主要机制。
Overpressure mechanism is researched from the aspects of compaction disequilibrium, hydrocarbon generation and rock salt sealing according to the geophysical and geochemical data.
低渗透性的沉积物在快速沉降过程中 ,上覆岩层产生的不均衡压实可产生相当大的超压 ,这是沉积盆地形成高压的主要机制。
Overpressure mechanism is researched from the aspects of compaction disequilibrium, hydrocarbon generation and rock salt sealing according to the geophysical and geochemical data.
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