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Position of the southern marginal suture of the East European Craton
Authors:V G Kazmin  L I Lobkovsky  N F Tikhonova
Institution:1.Shirshov Institute of Oceanology,Russian Academy of Sciences,Moscow,Russia
Abstract:Old and modern data are given and discussed. They allow us to decide where the real position of the south marginal suture of the East European Craton is. According to the geophysical and aerogeophysical studies, Paleozoic deposits of the Karpinskii Ridge are bedded upon deeply sunken continuation of Archean-Proterozoic complexes comprising the Voronezh massif and crystalline rocks belonging to the Astrakhan Dome. The latter have a pre-Riphean age. It is possible that the crust in the southeastern part of ridge in a narrow zone with >20 km depth of the basement surface (BS) and, partially, in the Sarpinskii trough has oceanic origin.
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