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.

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。

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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.

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。

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