Abstarct: Modeling and interpreting geophysical data have important role in the determining of appropriate drilling points. In this research, the combination of geological data such as mineralization and characteristics of copper ore deposit and geophysical data (Resistivity and Induction Polarization Methods (IP) in the Raen-Kerman region used for the invers modeling. Geophysical data in the Raen area consists 6 resistivity and IP profiles using by pole-dipole array in the southwest of the northeast trends .For this modeling have been used from the Res2dinv, ZondRes2d and Res3dinv softwares. The copper mineralization host rocks are volcanic and pyroclastic rocks that bearing propylitic, argillic and silica alterations. The structure of the mineralization occurs as vein which is formed by hydrothermal fluid through the joints and fractures. The mineralization occur as dissemination and veinlets in the previous fractures and include malachite, azurite and chalcocite. Geophysical surveys provide useful information about the mineralization in depth. Geophysical and geological studies could be determining the economic zones. Combination of these studies show the mineralization occurs in the 30 m depth. The results of the studies show that mineralization is mainly concentrated in the middle sections of the area.