Songgui bauxite deposit consists of 4 ore blocks, which all belong to the palaeo -weathering crust sedimentation type formed in the end of Late Triassic. They are formed in different stage of the similar sedimentary environment. The most advantageous area of sedimentary bauxite deposit is the upper subtidal-tidal zone. The ore deposit is affected by the palaeogeographic environment, palaeotectonic and lithologic character, etc.