牙哈断裂构造带位于塔里木盆地塔北隆起轮台断隆的中段北缘，受多期次构造运动影响该带内断裂异常发育,并且是控制寒武系白云岩裂缝型储集层发育的最主要因素，同时也是该带油气运移的主要通道。通过对断裂的精细刻画、对断裂系统的空间展布和断裂发育史的分析，对该带油气成藏规律和寒武系潜山勘探问题有了进一步的认识。

The Yaha fault structure belt is located in the north of the central Luntai anticline of the northern uplift of Tarim basin. Influenced by several tectonic movements, faults are widely developed and fault system is the most important factor that controls the development of Cambrian dolomite fracture reservoirs. In this paper, we analyze the developing time, space distribution and evolution history of the fault system which will contribute to oil and gas accumulation research and exploration of the Cambrian buried hill in this area.