褶皱运动(folding,folding movement)是指使岩层和面理发生反复褶皱的构造运动。在地壳强烈活动的地槽区,水平挤压产生的褶皱运动,导致线性褶皱带形成。
岩性圈闭和地层圈闭的形成与海平面变化和褶皱运动有关。
For lithologic and stratigraphic traps, their origination might relate to sea level changes and folding.
由于受区域构造长期作用的影响,在北天山山前地区逐步发育形成了多排褶皱背斜及活动断裂,且运动方式具有独特性。
Under the effect of regional tectonics there develop many raws drape anticline and active fault in the front of mountain and they have especial motion fashion.
由于受区域构造长期作用的影响,在北天山山前地区逐步发育形成了多排褶皱背斜及活动断裂,且运动方式具有独特性。
Under the effect of regional tectonics, there develop many raws drape anticline and active fault in the front of mountain, and they have especial motion fashion.
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