The technology of formal interpretation of deep geoelectrical parameters of the northern part of the Scythian Plate

MT/MV methods serve as a source of direct information on the presence of anomalies of electrical conductivity and geoelectrical parameters of the crust and upper mantle. Deep point MTS village Ridne locates in the northern part of the Scythian Plate. The qualitative characteristic of the experimental data suggests to possible presence of a conductor with S = 3000 – 4000S. Results of 1D- inversion indicate the existence of an anomalous zone with ρ = 100 Ohm∙m. The total longitudinal conductivity of the sedimentary strata along the ascending branches ρп reaches over 400 S. An analysis of the magnetic-variation responses shows a complex three-dimensional situation in the deep part of the Sivas through, that correspond to surface and deep electrical conductivity anomalies. This question needs to solve by three-dimensional modeling.