The Kuh-e Lakht region, part of the Central Iran Zone, is located in the Urmia-Dokhtar Volcanic Belt in the southeast of Tudeshk. Geological evidence indicates a high sulfidation epithermal mineralization system. In this area, geophysical studies including magnetometry survey with 900 points and IP/RS surveys are performed in two profiles with Pole-Dipole array. We perform 3D inversion of magnetic data and 2D modeling of IP and RS data of the two profiles and interpret results. The inversion results indicate that mineralization occurred at the boundary of the magnetic susceptibility variations corresponding to the reduction of resistivity. In addition, a high amount of chargeability due to the presence of argillic zone in the area is related to mineralization.