Xihu depression is a cretaceous - tertiary basin undergoing multi - episodic tectonism.

西湖凹陷是经历多期构造作用的白垩 - 第三纪盆地.

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Multi - episodic rifting and inverted tectonism caused complicated structural styles and geology structure.

多期裂陷和反转构造作用的叠加导致了相对复杂的构造格架样式和盆地地质结构.

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The palaeogeographical evolution sensitively responds to the tectonism in the whole Triassic.

绍兴?宜春断裂作为构造分区的界限,控制了其两侧古地理的发展.

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Hence, tectonism and sedimentation were main factors controlling multiphase hydrocarbon and multiphase pool - forming of the basins.

因此, 构造和沉积作用是控制该类盆地多期次成烃成藏的主要因素.

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