1. INTRODUCTION
Ground penetrating radar (GPR) is widely used for subsurface exploration. It is a non-destructive method and can obtain higher resolution images than other subsurface imaging method. Other than conventional subsurface imaging using the reflected signals from scatterers, GPR can also be used to estimate the distribution of propagation velocity of electromagnetic waves in subsurface structure. Previous studies show that common midpoint (CMP) velocities can be used for civil engineering applications, hydrogeological applications, and groundwater research [1]. Also, there are many kinds of research on road or pavement inspection targeting distortion or voids beyond the pavement layer [2] [3].