The easiest and cheapest method in geophysical operations for mining is the magnetic method. Different methods and filters are used to obtain more accurate results from the interpretation of the magnetic data which each of them has strengths and weaknesses. The most important goal in conclusion from an interpretation is to accurately determine the shape of the masses, their edges and their depth. In this study, reduction to pole filters, first vertical derivatives, and analytical signals are applied to determine anomalous boundaries and tilt-depth filters to determine depths of masses on magnetic data surveyed in the Tanorche Mine is located near Kashmar. By matching and overlapping the results of each of the filters compared to the other filters, the best results were obtained for delimiting deeper masses containing magnetite and deep slope. Depth estimation results show that most of the magnetite minerals that cause magnetic anomalies in this area are in the depth of 30 to 40 meters.