Abstract: In Daheshang mountain and adjacent area occurs an upper interlayer (or cover) gliding belt consisting of a series of imbricate overthrust faults, at their base exists a large main thrust withalow dip angle, occurring between the overlying soft cover and the underlying rigid rock basement. The gliding motion along this main thrust caused the geological structures to be formed between the cover and basement. But they differ from the structures formed in Pre-Sinian basement. The formation of this structural system in studied area can be considered as a reault of lateral compression in SEE and NWW directions. And the cover gliding probably started from Late Paleozoic and continued in Jurassic period or later.

摘要： 辽南大和尚山区及其邻区存在一个盖层滑移带,它在盖层中引起了一系列逆掩叠瓦状冲断层,并伴生有花岗质岩脉注入,为今后深入研究本地区构造提供了有利条件。