野外判定岩浆岩地区逆冲推覆构造的主要标志是逆冲叠瓦扇和软弱滑动层的存在。
The imbricate fan of thrusts and soft layer are main structure features distinguishing thrust-nappe structure in magma-tic body area.
三组室内模型试验表明具有软弱下卧层的地基破坏模型基本上属于冲切破坏。
Three sets of model test in laboratory show that the failure model in the foundation with soft clay underlying layer belongs basically to the punching shear failure.
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。
Fold-thrust belts and salt-related structures are very prevalent in the Kuqa foreland fold-thrust belt of Tarim Basin in Northwest China.
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