In order to explore the gold in the Barite veins, using geoelectric methods in a region in the city of Danesfahan, north of the Hassanabad fault, Appearance resistivity and induction polarization were conducted over several profiles perpendicular to the observed outcrops. Then collected data have been inverted using RES2DINV software to estimate resistivities and chargabilies of the subsurface. To reduce non-uniqueness of the problem and more constraining the inversion to the data both apparent resistivities and chargabilities are simultaneously are contributed to the inversion. Results of the inversion are presented in form of contouring sections. In the sections sudden variations of resistivities and chargabilities are related to discontinuities. Since main morphology in this area shows metal scattered mineralization, thus areas with high resistivities and chargabilities are indicated and identified as metal mineralization.