Abstract
Analysis of drilling data within the Orenburg sector of the northern marginal zone of the Caspian Basin and the Sol'-Ilets rise has shown that horizons of the Moscovian Stage of Late Carboniferous and Early Permian age rest on an eroded surface of Bashkirian deposits in a transgressive succession.Changes in thicknesses in the upper Paleozoic stratigraphic complexes indicate a significant discordance between the structural plans of the Artinskian and Bashkirian deposits and the possibility of discovering buried traps here, promising in the search for oil and gas.
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