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The article analyzes the development of sedimentation in a rather narrow interval of geological time: middle Devonian (397 mA) to early Carboniferous (345 million years old) on a large area of the North-Western periphery of the Bashkir arch. It is shown that the Paleozoic deposits of this time are developed in all areas of the Russian plate and the Volga-Ural oil and gas province. However, the distribution of oil and gas is highly differentiated in space. The authors try to find out the specifics of sedimentation and possible conditions of hydrocarbon generation. Oscillations of the world ocean along the Eastern margin of the Russian plate have an obligation paragenetically tectonic movement. The centre of sedimentation was the axial zone of the Kama-Kinel system of troughs located over areas of active rifting. This created the conditions

FEATURES OF THE DEVELOPMENT CARBONITESETUPLITE BASIN IN LATE DEVONIAN - EARLY CARBONIFEROUS IN THE NORTH-WEST OF THE BASHKIR ARCH