侏罗山式褶皱

江苏靖江&苏州地区侏罗山式褶皱及滑脱断层的研究

Studies on the jura type fold and the decollement fault in jingjiang suzhou area , Jiangsu Province

川东侏罗山式褶皱的数值模拟及成因探讨

Numerical Modeling and Formation Mechanism of the Eastern Sichuan Jura-type Folds

黔东南地区褶皱构造样式及其断层突破模式川东侏罗山式褶皱的数值模拟及成因探讨

Structural Style and Thrust Breakthrough Model of Fold in Southeast Guizhou

川东侏罗山式褶皱带形成时代：不整合面的证据

The Folding Time of the Eastern Sichuan Jura-type Fold Belt : Evidence from Unconformity

其主要类型有席状逆冲构造、侏罗山式褶皱推覆构造、楔状推覆构造及剪切褶皱逆冲构造等。

The main kinds of the nappes are sheet thrust , Jurassian fold nappe , wedge-shaped nappe and shearing fold-thrust structure , etc.

祁阳弧的成型和侏罗山式褶皱的发育，是在东西向挤压应力场作用下，盖层与前泥盆系基底之间的滑脱造成的。

The shaping of Qiyang arc and the development of Jura-type folds are resulted from the decollement between pre-Devonian basement and its cover under eastwest compressive stress field .

这种有序变形规模巨大，仅川东的隔挡式褶皱冲断带规模就超过了著名的侏罗山式褶皱。

This regulated deformation is considerable in scale , and hence the partition wall style fold-thrust belt in the east of Sichuan is much bigger than the famous Jurassic style folding .

从几何学研究表明表层构造具有侏罗山式褶皱的特征，同时揭示其下必有滑脱断层的存在。

According to geometrical study , it shows that the surface geological structures in this area are characterized by the Jura-type fold and reveals that decollement fault is certain to be in existence beneath the structures .

通过构造解析划分出了顺层韧性剪切带、阿尔卑斯式褶皱、侏罗山式褶皱、过渡性剪切带、逆冲推覆构造及地垒-地堑式构造等组合类型。

According to the structural analysis , these have been divided into several composed types such as bedding ductile shear zone , Alpinotype folds , Mt Jura_type folds , transition shear zone , obduction nappe structure and horst_graben structure .

南昆仑造山带西段发育逆冲推覆构造、平行走滑构造、地垒&地堑构造和阿尔卑斯式褶皱、侏罗山式褶皱，前两类构造尚有韧性剪切带伴生；

Lied at the western section of south Kunlun orogenic zone , there developed with the thrust nappe structure , parallel glide structure , horst-crabon structure , Alpine-type folds and Jurassic folds , the former two sorts of structures still have been accompanied by ductile shearing belts ;