地壳构造的

Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期生的盆地底板，将显示地壳构造的等级次序和造陆性质。

The episodic flow of hydrocarbon migration and all geofluid and the episodic action of crust structure are complementary to each other and mutually determined.

油气式运移与地流体的式流动都与地壳的式构造活动相辅相、互为因果。