The article presents the results of studies of the geoelectric structure of the Uimon depression of the Gorny Altai using the complex of geoelectric methods, which includes electromography, vertical electrical sounding and transient electromagnetic sounding. According to the data of the complex, the near-surface and deep geoelectric characteristics of sedimentary filling were obtained.
The article presents the results of the study of electrical anisotropy by two methods of DC (vertical electrical sounding and electrical tomography) in the area of the Bystrovka field area, on the shore of the Novosibirsk reservoir. Taking into account a priori well data, the parameters of the geoelectric model and the anisotropic characteristics of the section are determined. On the site of the study, according to the data of two methods, electrical anisotropy observed in the reference geoelectric horizon, represented by shale. In addition, the main direction of crack propagation is determined.
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