The ne - strike compressional faults are not intersected with the ew ma in fault zone , but a kind of transform structure resulted from its right lateral strike slip , and one of the typical example is the mesozoic thrust systerm in the northeast side of the main fault in western liaoning 在青龍斷裂帶兩側(cè),分布有許多北東向壓性斷層,它們與東西向主斷裂帶不是簡單的切割關(guān)系,而是東西向主斷裂帶右行走滑活動中的分支斷裂,位于青龍斷裂帶北東側(cè)的遼西地區(qū)中生代逆沖推覆構(gòu)造,也是青龍斷裂帶在右行走滑作用下,因構(gòu)造方向的改變發(fā)生構(gòu)造轉(zhuǎn)換的結(jié)果。