Helan cold rift valley is located between north Qilian orogenic belt and southwest margin of North China plate. Based on continental shelf, continental slope transition zones and basal structure of superposed basin and its bordering fault zone and refers to geophysical information in the area, it is determined that the boundary of Helan cold rift between North Qilian orogenic belt and North China Plate is located in Qingtongxia (Niushou Mountain)-Guyuan fault belt. In the long tectonic evolution, it is characteristic of multi-directionality, multistage and multiplicity.