Linear anomalies of magnetic and gravitational fields on Voronezh Crystalline Massif
The authors analyze the morphology of gravity and magnetic field anomalies, as well as vertical gravity gradient within Voronezh Crystalline Massif (VKM). It is shown that gravity gradient measurements added to the complex of conventional gravimagnetic observations provide an increase in the reliability of geologic interpretation. The complex interpretation of gravimagnetic fields in combination with gradient measurements made it possible to distinguish, apart from a system of orthogonal N-W and N-E anomalies, a meridional-latitudinal system of anomalies.