EVOLUTION OF GEODYNAMIC CIRCUMSTANCES OF EAST EUROPEAN PLATFORM AND ITS FRAMING IN PHANEROZOIC AND ASSOCIATED MINERAGENIC TRANSGRESSIONS
Formation of the ancient platforms type economic deposits of cupriferous sandstones, rock and K-Mg salts, bauxites, Ti-Zr leads, associates tight with specificities of their geodynamic circumstances. The EEP geodynamic regime in Phanerozoic is the most merciful for exogenous ore lodes. In Late Permian it spreads upon contiguous areas of West Europe that provides formation of numerous exogenous platform type ore objects there. This phenomenon is termed as «mineragenic transgression». In geological histories of EEP and in comparison others Earth's platforms note changeability of contours, domination of the destructive type processes, appearance on newly activated areas of ore objects more peculiar for TTT (Tectonic-Thermal Transformations) belts. Evolving conception seems to be applicable for the Voronezh anteclise, especially its south-eastern the Donbass contiguous areas.