Pore fluid pressure can do favor to rocks rupture, while tectonic movement is the main factor that induces the rupture of source rock and the episodic fluid migration.
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美
- 孔隙流体压力有利于岩石产生破裂,但是中央隆起带的构造活动是造成岩石破裂、流体瞬态运移的主控因素。