幕式流动是油气运移的最大特征，与盆地的幕式构造活动相辅相成互为因果。
Episodic flow is the most characteristics of hydrocarbons migration and complement each other and inter determined with the episodic movement of sedimentary basin structures.
地壳深部的变质流体可能也是呈幕式活动并产生幕式的构造运动。
The metamorphic fluid activity in the deep parts of crust can be in episodic manner and produce episodic tectonic movements.
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