The gradient of the tectonic additional hydrostatic pressure is the main cause of the long-distance migration of the fluid, oil and gas.
构造附加静水压力梯度是流体及油气长距离水平运移的主要原因。
It is in disputed that how much additional tectono-induced hydrostatic pressure can be produced by tectonic difference stress.
构造差应力究竟能够产生多大的附加静水压力在地学界一直有很大争议。
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