There is the special structure combination and the concentration of strong earthquake in the Pu'er block. The geology phenomena of motion and deformation caused by motion of the active fault and the sub-block which brings the extensive attention and further research to the scholar of geological society. Basing on the past research achievements,we will construct the 2 dimensional shell finite element model of Pu'er region containing the active fault. Applying the velocity of block per year measured by GPS data and the researches on the geology and geomorphology as the boundary conditions of finite element model,we then compute the spatial distribution of deformation in the Pu'er region and simulate the deformation displacement along the NEE and NNW direction. Lastly,we analyze the characteristics of horizontal and vertical displacement field in the Pu'er region. The numerical result shows that extension motion of the southeastern margin of the Qinghai-Tibetan Plateau makes the movement of slump due to the gravity. In the research area,the motion of fault with NEE strike draws the fault with the NNW strike to move in conjugation direction. The vertical deformation caused by the uplift movement is agreed with the result of 60 years of larger regional leveling and the deformation along the NNW direction is distributed irregularly which is made possible by the regional stress accumulation and adjustment after the earthquake. The deformation field along the NEE direction is larger in western part of Pu'er region than that in eastern part,especially the northwest part of region which is corresponding to the recent Jinggu MS6.6 earthquake. Lastly,we analysis preliminarily the dynamic problems in research area.