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.
如同倒转褶皱一样，平卧褶皱构造其中一翼的岩层层序是倒转的。
Like overturned fold, the rock sequence of one limb of the recumbent fold is overturned.
早期韧性简单剪切机制下产生的平卧褶皱，经后期挤压再次发生褶皱，显示构造运动的多期性与构造环境的复杂性。
Recumbent folding was formed by simple ductile-shear dynamics in the early stage, which was refolded by succeeding compression, showing the complexity of multiphase tectonics.
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