The traditional version of tracing discontinuous dislocations on the materials of gravity reconnaissance involves the transformation of the anomalous field into a field of complete horizontal gradient. In the presence of a complex, differently oriented fault system, the integral nature of the gravity field significantly complicates the solution of the problem. For such geological conditions, the anisotropic transformation method, which is characterized by greater efficiency and resolution, is proposed. The main characteristics of anisotropic transformation and recommendations on the choice of optimal transformation parameters are given.
