Computers & Geosciences, Volume 84, November 2015, Pages 1–9
Julia B. Curto, Tatiana Diniz, Roberta M. Vidotti, Richard J. Blakely, and Reinhardt A. Fuck
“We offer a methodology to analyze the spatial and statistical properties of the tilt derivative of magnetic anomalies, thus facilitating the mapping of the location and depth of concealed magnetic sources. This methodology uses commonly available graphical information system (GIS) software to estimate and interpolate horizontal distances between key attributes of the tilt derivative, which then are used to estimate depth and location of causative bodies.

Fig. 8. (a) Reduced-to-pole magnetic anomaly field of the study area. (b) Main geological features of the northwest Paraná Basin. The Arenópolis magmatic arc and the Paraguay Belt represent the Neoproterozoic basement of the basin. Dashed black lines are magnetic lineaments (Curto et al., 2014): (A) Serra Negra, (B) Baliza, (C) General Carneiro.
“Application of the method to synthetic data illustrates its reliability to determine depths to magnetic contacts. We also achieved consistent depth results using real data from the northwest portion of the Paraná Basin, Brazil, where magnetic anomaly interpretations are complicated by low geomagnetic inclinations and rocks with remanent magnetization. The tilt-derivative method provides more continuous and higher resolution contact information than the 3D Euler deconvolution technique.”