CHARACTERISTICS OF FAULT SYSTEM IN YAHA STRUCTURE BELTOF NORTHERN UPLIFT, TARIM BASIN
塔里木盆地北部隆起牙哈构造带断裂特征

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 area.