Fitting algorithm for surfaces of anomalies based on the analysis of the gravity gradient vector
The construction of 3D models of Earth anomalies is an important scientific and practical task. The article describes the developed algorithm for recognition and fitting the surfaces of anomalies. The initial data are the values of the gravity gradient vector specified at the nodes of a 3D regular network. A step-by-step algorithm and its variable parameters are described in detail. The algorithm can be used not only for the processing of gravity data, but also for solving some of the problems that analyze vector physical parameters in 3D space.