In this study, the exploration area around the Bakhleh area in Kamyaran city was investigated using the magnetometric method. A Proton magnetometer was used to collect the data. Geological studies of the area indicate the mineralization of copper in the form of carbonate and sulfide in the ultramafic fields as well as the mineralization of iron in the form of oxide and hydrated minerals. Magnetic data were collected at a distance of 20 meters in the north-south direction, which was a total of 332 data points. The obtained results are presented in the form of magnetometric maps. These maps show the general trend of changes in areas prone to iron mineralization. The results of range magnetometry show that there are fractured fault zones along the approximate north to south with high magnetic anomalies.