New Data on the Sezym Formation (Lower Permian, Polar Urals)

Resumo

New data on the composition and structure of the Sezym Formation of the Lower Permian on the western slope of the Polar Urals are presented. This formation rests disconformably on the Middle Carboniferous shallow marine limestones and is conformably overlain by the Artinskian deep marine clastic deposits. New data are important for the reconstruction of the Late Paleozoic paleogeography and the geodynamic setting of the northeastern sector of the European Craton.