“…to find the density of the source masses from the given gravity field functionals, such as norm of the gravity vector (from gravimetry), gravity vector (from the inertial systems or astronomical observations plus gravimetry), gravity potential (from geodetic leveling), on or above the surface of the earth, is of particular interest for geoscience studies. For this reason extensive contributions are made in this respect that as recent examples we refer to Welford et al (2010), Aitken (2010), Schreiber et al (2010), Kimbell et al (2010), Welford and Hall (2007), Jacoby et al (2007), Camacho et al (2007), Ebbing et al (2007), Bosch et al (2006), Strykowski et al (2005), Tiberi et al (2005), Pinto et al (2005), Jacoby and Çavşak (2005), Cai and Wang (2005), Kaban et al (2004), Wang et al (2004), Widiwijayanti et al (2004), Çavşak et al (2002), Koslovskaya et al (2004), Rivero et al (2002), , Silva et al (2001Silva et al ( , 2002Silva et al ( , 2007, Tondi et al (2000).…”