Based on seismic and well data, the salt structure styles, formation mechanism and influence on regional tectonics of Tabei Uplift is investigated in this paper in Yingmai 2 work district, Yingmaili area, western Tabei Uplift. It is implied that western Tabei Uplift underwent strike slip movement in Late Paleozoic when salt deformation took place. Salt structures were deformed in compressional tectonic setting in Late Paleozoic and, according to the analysis of the structural evolution section, the main fault was remobilized as a synsedimentary fault in Triassic with a limited scale. After Triassic these structures were relatively stable. Salt layers significantly influenced the tectonic deformation. In structural layers below and above them, inharmonious structure styles were formed.