收缩挤压着表层使得部分地壳压在其余部分形成了这样长长而弯曲的悬崖。
This contraction compressed the surface and thrust some sections of crust over others, creating long curving cliffs like the one shown here.
这些伸展构造很显然是扬子克拉通和华北克拉通在三叠纪碰撞时，大别山造山带前陆位置岩石圈弯曲导致地壳上部产生非弹性变形的结果。
Such structure in the collision foredeep of the Dabieshan Orogen was resulted in inelastic extensional deformation of the conver side of the flexed plate aroused by lithospheric flexure.
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