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The main purpose of the paper is the identification and analysis of the anisotropic characteristics of the geoelectric section in the area of research in the village Mukhor-Tarkhan. The choice of the anisotropic model is justified a priori extensive geological, hydrogeological and geophysical information about the structure of the site. Found that the temporal variations of the coefficient of anisotropy, resulting from interpreting geoelectric data, characterize the ongoing aftershock process and can be used for problems of electromagnetic monitoring of seismotectonic processes