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Recent seismic surveys and reprocessing by Sevoteam/MAGE make it possible to verify and add information about the sedimentary cover especially Lower Paleozoic terrigenous and carbonate complex (Cambrian-Lower Permian) within the southern part of the Barents Shelf, including the aquatorial continuation of the Pechora Platform, Kola-Kaniri Monocline, South Barents Basin, West-Kola Saddle and other structures.