组成地壳的岩层，受构造应力的强烈作用使其发生波状弯曲而未丧失其连续性的构造，称为褶皱构造。褶皱构造是岩层产生塑性变形的表现，是地壳表层广泛发育的基本构造。
It suffered multi-period and multilevel deformation in Foping area, and the structural characteristics here show a series of fold structure, which spreads nearly east-west and reflects a strong north-south compression.
该区现今的主体构造主要表现为一系列东西向展布的褶皱构造,反映了强烈的南北向挤压作用。
参考来源 - 南秦岭佛坪隆起的构造过程及成因机制·2,447,543篇论文数据，部分数据来源于NoteExpress
与断裂相伴的褶皱构造沿断裂走向分布，且受断裂活动控制。
Fold structure associated with the fault distributed along fault strike, controlled by faulting.
全球褶皱构造带的空间分布规律完全符合这种地球物理机制。
The space distribution regularity of global folded tectogene is well agreed with the geophysical mechanism.
如果褶皱构造的轴面基本上是水平的，那么我们称它为平卧褶皱。
If the axial plane of a fold is essentially horizontal. Then we call it recumbent fold.
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