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 pn 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.
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机译：MT / MV方法用作关于存在外壳和上部地幔的电导率和电气参数的异常的直接信息的来源。 Deep Point MTS Village Ridne位于斯中斯北部的北部。实验数据的定性特征表明，可能存在具有S = 3000-4000s的导体。 1D-反演的结果表明，存在异常区，ρ= 100欧姆·m。沿升枝PN的沉积地层的总纵向导电率达到400秒。磁场变异响应的分析显示了Sivas的深部中的复杂三维情况，对应于表面和深度电导率异常。这个问题需要通过三维建模来解决。
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