The landslide phenomenon of slope at the syncline core of Fujunchang by fast channel in Tianfu New Area of Meishan is analyzed. It is believed that the cause of landslide is the development of mudstone in the slope stratum, and the rock mass is broken with poor integrity because of syncline effect of Fujunchang. The excavation of the slope is too steep and is affected by the rainfall in the construction. In order to determine the treatment scheme, the sliding surface parameters are achieved according to the geotechnical test result and inversion result. The stability analysis and thrust calculation of the landslide are carried out. Finally, it is determined to use the treatment scheme properly for lifting the longitudinal slope and then clearing the earthwork.