The article considers the possibility of identifying of an inheritable character of the geodynamic situation and elements of structural and compositional complexes involved in the geological development of the Caucasus on geoelectrical and seismological depth sections in order to create a geological and geophysical model of the Earth's crust along regional profiles. Modern structural-tectonic, structural and compositional complexes of the eastern part of the Central Caucasus are interpolated with the main structures of the consolidated crust and lower crust. The correlation of deep crustal and mantle structures with deposits of solid minerals and hydrocarbons and the role of Moho discontinuity in the localization of deposits are of scientific and practical interest.
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