Yanyuan—Xichang—Zhaojue—Mahu wide-angle reflection/refraction deep seismic profile has been completed in the southeastern boundary region of Sichuan-Yunnan active block.The images of P-wave velocity structure and the basement interface along the profile are obtained by interpreting the arrival times of refracted Pg wave and using finite difference inversion and time-term inversion.The result shows that the basement structure is significantly inhomogeneous and different tectonic zones reveal different deformation features.