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.
虽然目前难以求得数值特解，但可用图解表示岩席应变状况、构造变形特点，估算拆离滑脱带最大埋深和计算盖层的绝对缩短量。
Although it is difficult to get numerical solution up to date, the sheet strain and the characters of the structural strain can be illustrated by graphic solutions.
在岩块拆离滑脱过程中所形成的主拆离滑脱带、次级拆离滑脱带及层间滑动断裂成为较发育的构造扩容空间。
The main and second detachment belts as well as interformational faults were formed during the gliding of rock masses, and became well developed structural expanding space.
应用推荐