“…The magnetic method has a well-established role in the interpretation of the complex structure, tectonic framework, faults, shear zones, and fractures (e.g., Verduzco et al, 2004;Wijns et al, 2005;Anudu et al, 2012;Khalil, 2012;Khalil, 2013). Variety of semiautomatic filtering techniques based on the derivatives of the magnetic data has been developed for determination of the magnetic source parameters such as locations of boundaries and depths (e.g., Petar Stavrev, 2006;Furness, 2007;Khalil, 2013).…”