The authors used the radar data from the satellite ALOS/PALSAR of oft-com:office:smarttags" />Japan and the differential interferometric synthetic aperture radar (D-InSAR) technology to derive the coseismic displacement field produced by the MS 8.0 Wenchuan earthquake. Based on processing SAR data of 7 tracks and 112 scenes by the two-pass method, the authors obtained the interferometric map of 450 km×450 km covering the causative fault and determined the distribution range of incoherent zones. The result shows that the Wenchuan MS 8.0 earthquake has produced a vast area of surface deformation along the Yingxiu-Beichuan Fault, primarily concentrated in a near-field range of 100 km wide on the both sides of the causative fault.