倒转褶皱

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 .

毛集&二郎坪断陷带中的主体构造格架是复式倒转褶皱系。

The main structural framework of the Maoji Erlangping down faulted zone in Henan is represented by a composite overturned fold system .

倒转褶皱的粘性流体有限元分析

Finite element analysis of an overfold using the viscous fluid model

本区构造形态以推覆岩片大量叠置、平卧与尖棱倒转褶皱复合为特征，属板块聚合带成分。

The composition is of plate convergence belt .

这种类型的褶皱构造叫做倒转褶皱，因为褶皱其中一翼的岩层层序已随褶皱作用发生倒转。

We call it overturned fold because the bedding sequence of one limb is overturned due to folding .

造山运动末期，发育浅层次韧脆性开阔褶皱、区域性同斜倒转褶皱及逆冲断层。

In the ending stage of orogeny , upper level ductile - brittle broad fold , regional homoclinal - overturned fold and brittle obduction occured .

该带同样发育一系列斜歪褶皱和倒转褶皱，褶皱的位态和形变机制与整个推覆构造的受力机制相吻合。

This belt also developed a series of oblique and overturned folds . The bit-state and deformation mechanism of the fold anastomosed with the whole nappe .

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 .

华力西&印支期发展演化为裂陷带，并褶皱造山使裂陷带南北向大规模收缩，形成复式倒转褶皱系。

During the Hercynian-Indochina epoch the marginal fault depression basin developed into a fault zone with strong press of north-south direction and formed a folded chain consisting of inverted composite fold system .

在地质演化过程中，渣尔泰山群主要经历了3期褶皱变形，即早期的层内褶皱，主期同斜倒转褶皱与晚期叠加褶皱。

In the geological evolution of the fold structure , this suite of strata experienced three stages of fold deformation : the intraformational fold in the early stage , the homoclinal reverse fold in the major stage , and the superimposed fold in the late stage .