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.
如果倒转褶皱构造的两翼倾角相等，则可称这种特殊类型的倒转褶皱为等斜褶皱。
If both limbs of overturned fold have same dip Angle we call this special overturned fold isoclinal fold.
由北向南分为前缘挤压滑脱构造带、斜歪倒转褶皱—逆冲断层带和逆冲推覆岩席及叠瓦状逆冲断层带。
From north to south, several tectonic belts can be distinguished: front compressive detachment belt, overturned thrusting belt, sheeted thrusting belt and imbricate thrusting belt.
根据变形力的强度，褶皱可以是平缓的，陡峭的，倒转的，或逆掩的。
Depending on the intensity of the deforming forces the folds may be gentle sharp overturned or overthrust.
根据变形力的强度，褶皱可以是平缓的，陡峭的，倒转的，或逆掩的。
Depending on the intensity of the deforming forces the folds may be gentle sharp overturned or overthrust.
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