“…The EUD method is based on the Euler homogeneity relation (Thompson, 1982) and is employed to estimate the accurate origin and depth of the potential field source. Since the 1990s, 2D and 3D implementations of EUD on gravity and magnetic potential sources have been widely used (Reid et al, 1990;Paterson et al, 1991;Roest et al, 1992;Beasley and Golden, 1993;Hearst and Morris, 1993;Fairhead et al, 1997;Zhang et al, 2000;Mushayandebvu et al, 2001;Silva et al, 2001;Silva and Barbosa, 2003;Fitzgerald et al, 2004;Keating and Pilkington, 2004;Al-Saud, 2014;Ekinci et al, 2017). This method uses potential field data and their first-order derivatives in a system of linear equations.…”