Abstract:According to the gravitational and aeromagnetic interpretation, there exist six larger-scale tectonic belts of EW direction in the crust in the northeastern Qinghai-Tibet Plateau, which have common features as follows:1) they all extend more than 1000 km from east to west and about 60 km from north to south. 2) the deeper it is, the more outstanding the EW directional tectonics is. 3) the central distance between the adjacent tectonic belts is 1°20' and has a equidistant feature. 4) there are also secondary tectonic, belts in EW strike beyond,the large-scale belts. The stong earthquake activities in the northeastern Plateau are closely related to the EW trending tectonic belts. The close relationship results from the left-lateral shear motion of EW structures under acting of the, principal compressive stress in the NE direction.