倒转褶皱是指轴面倾斜，两翼向同一方向倾斜，一翼产状正常，另一翼产状倒转的褶皱。
风成沙丘普遍存在角砾前积、拖曳褶皱和倒转褶皱等同沉积变形构造。
The synsedimentary deformation structures are common in eolian dunes, such as brecciated foresets, drag folds and overturned folds.
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.
本文采用有限元方法，分析单层对称褶皱作用和一个天然倒转褶皱的变形过程。
Symmetrical folding of a single layer and folding process of an overfold are analyzed by using the finite element method.
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