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西秦岭地区在印支期受南北方向的挤压 ,北东向逃逸构造较为发育 ,通过几何学、应变学、运动学等特征的研究 ,认为逃逸构造是造山带中重要的构造格架 ,而滑覆是其主要机制
The West Qinling area was squeezed north-south direction during the Indosinian and the northeasterward escape structure was relatively developed. Based on the studies of geometry, strain and kinematics, it is considered that the escape structure is an important tectonic framework in the orogenic belt Slipcover is its main mechanism