The Chuanlinggou Formation of the Mesoproterozoic stratum which developled in the northern part of the North China Paleocontinent was the turning point which the sedimentary system change from littoral neritic terrigenous clastic rocks to epicontinental sea carbonatite rocks. Though some liquefaction structures which developed at the bottom of the Chuanlinggou Formation have been performed to reveal the seismogenic origin, but very few work on other soft sediment deformation structures, such as hydro plastic deformation and fluidization have been done. We study such a comprehensive study on types, features, layers, and spatial location of soft sediment deformation structures developed in the Chuanlinggou Formation has great significance for understanding the characteristics of fault activity in prototype basin.