(1) Li Xiong, 2003. On the use of different methods for estimating magnetic depth. The Leading edge. P1090-1099.
(2) Peters, L. J. 1949. The direct approach to magnetic interpretation and its practical application. Geophys. V. 14 ,P 290-320.
(3) Bean, R.J. 1966. A rapid graphical solution for the aeromagnetic anomaly of the two-dimensional tabular body. Geophys. V. 31,P. 963-970.
(4) Naudy, H. 1971. Automatic determination of depth on aeromagnetic profiles. Geophys. V. 36, P.717-722.
(5) Murthy, I.V.R., Rao Viswesara, C. and Krishna, G. G. (1980). A gradient method for interpreting magnetic anomalies due to horizontal circular cylinder, infinite dykes infinite dykes and vertical steps. Proc. Indian Acad. Sci. V. 89, P. 31-42.
(6) Ku,C.C. and Sharp,J.A. 1983. Werner deconvolution for automated magnetic interpretation and its refinement using Marquardt's inverse modeling. Geophys. V. 48, P.754-774.
(7) Atchuta Rao, D, Ram Babu, H.V. and Sankor Narayan, P.V. 1981. Interpretation of magnetic anomalies due to dikes: The complex gradient method. Geophys. V.46, P.1572-1578.
(8) Roest, W.E. and Verhoef, J. 1992. Magnetic interpretation using 3-D analytical signal. Geophys. V.57, P. 116-125.