Fig. 2From: 2.5D regularized inversion for the interpretation of residual gravity data by a dipping thin sheet: numerical examples and case studies with an insight on sensitivity and non-uniquenessModel 1: noise-free data. Top panel: preliminary (initial) inversion results obtained from the steepest descent (SD) method. Bottom panel: final inversion results obtained from the Gauss-Newton (GN) method which used the inversion results produced from the SD (top panel) as initial guess; see the text for details. Bottom panel shows that the observed and predicted data are coincident with each otherBack to article page