Estimating the location of a causative body from a self-potential anomaly using 2D and 3D normalized full gradient and Euler deconvolution

Abstract

Changes in the size and depth of sources greatly affect self-potential (SP) anomalies. Therefore, it is important to determinethe location of the source accurately. In the present study, applications of the normalized full gradient (NFG) method and Eulerdeconvolution (EUD) were described to determine the location of the sphere-like SP body as complementary approaches to otheroptimization algorithms. The NFG and EUD methods were tested on synthetic, noise-free, and noisy anomalies caused by sphere-likemodels in two-dimensional (2D) and three-dimensional (3D) cases. Subsequently, the methods were applied to real field data. Theimportance of the present study lies in the fact that it is the first 3D application of these methods to the SP anomaly caused by thesphere-like model in the literature. In order to determine the optimum harmonic number in the NFG method, a new criterion was usedinstead of the usual trial-and-error method, providing more reliable selection possibilities. In a similar way, average values were usedto determine the window size accurately in the EUD method. The test results of the synthetic and real field models were satisfactory.They showed that both methods are applicable to determine the location of sphere-like structures, such as ore deposits, in self-potentialsurveys.