Telford, W.M., Geldart,L.P.,&Sheriff,R.E. (1990). Applied Geophysics.2nded.Cambridge U. Press, Cambridge, U.K.
[2] Bleil, V., & Petersen, N.(1982). Magnetic properties of natural minerals.Paramagnetism. In: Landolt-Boernstein, Numerical data and functional relationships in science and technology,Springer Verlag Berlin, Group V, 1b, pp. 312-320.
[3] Dortman, N.B.(1984). Physical properties of rocks and mineral deposits (in Russian).Nedra, Moscow.
[4] Cisowski, S.M., & Fuller, M.D.(1987). The generation of magnetic anomalies by combustion metamorphism of sedimentary rock, andits significance to hydrocarbon exploration. Geol. Soc. Amer. Bull., 99, pp. 21-29.
[5] Nawrocki J., Wojcik A., & A. Bogucki. (1996).The magnetic susceptibility record in Polish and Ukrainian loess-palaeosol sequences conditioned by palaeoclimate. Boreas 25, pp. 161-169.
[6] Evans M. E., & Heller F. (2003). Environmental magnetism. Principles and Applications of Enviromagnetics, Academic Press, Elsevier, pp. 293.
[7] Plimer, I.R.(1985). Submarine exhalative ores.Geol. Survey of Czechoslovakia, pp. 394, Prague.
[8] Ellwood, B.B., & Wenner, D.B.(1981). Correlation of magnetic susceptibility with 180/160 data in late orogenic granites of the southern Appalachian Piedmont.Earth Planet. Sci. Lett., 54, pp. 200-202.
[9] Rochette, P.(1987a). Magnetic susceptibility ofthe rock matrix related to magnetic fabric studies. J. Struct. Geol., 9, pp. 1015-1020.
[10] Hrouda, F., & Kahan, Š. (1991). The magnetic fabric relationship between sedimentary and basement nappes in the High Tatra Mountains, N. Slovakia. J. Struct. Geol., 13, pp. 431-442.
[11] Heller F., Strzyszcz Z., & T. Magiera. (1998). Magnetic record ofindustrial pollution in forest soils of Upper Silesia.Jour. Geopfys. Res. 103, pp. 17767-17774.
[12] Müllerová, J., & Müller, K.(1972). Demonstration of the existence of two lava flows in the VelkýRoudný at SlezskáHarta (in Czech). Sbor.věd. prac. VŠB, 18, pp. 97-100. Ostrava.
[13] Grant, F. S., & West, G. F.(1965).Interpretation theory in applied geophysics, McGraw-Hill, New York, NY.
[14] Chandler, V. W., & Malek, K. C.(1991).Movingwindow Poisson analysis of gravity and magnetic data from the Penokeanorogen.east-central Minnesota, Geophysics, 56, pp. 123-132.
[15] Chandler, V. W., Koski, J. S., Hinze, W. J., & Braille, L. W.(1981). Analysis of multisource gravity and magnetic anomaly data sets by moving-window application of Poisson theorem, Geophysics, 46, pp. 30-39.
[16] Cordell, L., & Taylor, P. T.(1971). Investigation of magnetization and density of a North American seamount using Poisson’s theorem. Geophysics, 36, pp. 919-937.
[17] Garland, G. D.(1951).Combined analysis of gravity and magnetic anomalies. Geophysics, 16, pp. 51-62.
[18] Mendonca, C. A.(2004). Automatic determination of the magnetization to density
Boroomand et al. / Int. J. Min. & Geo-Eng., Vol.49, No.1, June 2015
66
ratio and magnetization inclination from the joint interpretation of 2D gravity and magnetic anomalies, Geophysics, 69, pp. 938-948.
[19] Doo, W. B., Hsu, S. K., Tsai, C. H., & Huang, Y. S.(2009)Using analytic signal to determine magnetization/density ratios of geological structures.Geophys. J. Int., 179, pp. 112-124.
[20] Mendonca, C. A., Meguid, M. M. A.(2008).Programs to compute magnetization to density ratio and the magnetization inclination from 3-D gravity and magnetic anomalies. Computer and Geosciences, 34, pp. 603-610.
[21] Hildebrand, T.G.(1985). Magnetic terranes in the central United States determined from the interpretation of digital data, inThe Utility of Gravity and Anomaly Maps,ed. Hinze, W.J., Soc. Exploration Geophysics, Tulsa,pp. 248–266.
[22] Alamdar, K., Ansari, A. H., &Kamkare-Rouhani, A. (2011). Using analytic signal in determination of the magnetization to density ratio (MDR) of the geological bodies. Earth and Space Physics journal, 38(2), pp. 167-182.
[23] Jekeli, C.,Erkan, K., Huang, O.(2010). Gravity vs Pseudo-Gravity: A Comparison Based on Magnetic and Gravity Gradient Measurements. International Association of Geodesy Symposia, 135, pp 123-127.
[24] Agarwal, B.N.P., &Lal, T. (1972). A generalized method of computing second derivative of gravity field. Geophysical prospecting, 20, pp. 385-394.
[25] Gunn, P.J. (1975).Linear transformations of gravity and magnetic fields. Geophysical Prospecting, 23, pp. 300-312.
[26] Mickus, K.L., Hinojosa, J.H. (2001). The complete gravity gradient tensor derived from the vertical component of gravity: a Fourier transform technique. Journal of Applied Geophysics, 46,pp. 159–174.
[27] AllahTavakoli, Y., & Safari, A. (2012). Surface Mass-density Determination of the Inversion of Land-based Gravitational Data