The experience of deep section compiling along DSS and CDP profiles testifies that these different seismic data can be interpreted within the framework of unified radial-zoning model of the lithosphere. The development of representative net of reference sections of the lithosphere has opened the way to the construction of a deep structure map. Their fundamental content is the interpretation of spatial distribution of structural-metrological units as results of paleoplates accretion in the process of Precambrian and Phanerozoic evolution. Conceptual – tectonics approach to the processing and analysis of the geophysical information enables approaching to problems of regional mineragenic prediction using structural and geodynamic factors. The latter are characterized by stronger correlation with distribution of leading types of mineral deposits as compared with geophysical data.


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