They were formed through regional isostatic adjustment and Theological flexure under the load of fold-thrust belts.
它是在褶皱冲断带负载的作用下，岩石圈通过区域性均衡调整及流变挠曲而形成的。
The main kinds of the nappes are sheet thrust, Jurassian fold nappe, wedge-shaped nappe and shearing fold-thrust structure, etc.
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。
Fold-thrust belts and salt-related structures are very prevalent in the Kuqa foreland fold-thrust belt of Tarim Basin in Northwest China.
褶皱-冲断带和盐相关构造均十分发育的秋立塔克地区构造极其复杂，该地区新生界内部存在两套起滑脱层作用的膏盐层。
应用推荐