学科断块构造说 层间滑动断裂词目层间滑动断裂 英文interlayer gliding fault
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.
层间滑动破碎带、岩体接触面和断裂构造是主要的含矿构造，它控制了矿体的形态和产状。
The main ore-bearing structure are the interlayer-gliding fracture zone, contact area of rock mass and fracture structure, which controlled the shape and the occurrence of orebody.
在西山和王家沟一带，为一套向北陡倾的反射层系和一组沿层间滑动的断裂；
In the Xishan and Wangjiagou area, it shows a set of steeply north-dipping reflective layers and a group of faults slipping along the layers.
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