Abstract
The Bazhenov high-carbon formation is a part of the Bazhenov formation, characterized by a high content of aquagenic organic matter. Formation is a perspective source for expanding the hydrocarbon resource base. The article presents a combination of the results of core studies, interpretation of well logging and seismic data. A multi-faceted approach to the study of rocks made it possible to divide the West Siberian basin into 13 structur- al-facies zones, each of which has its own structural features of the bazhenov high-carbon formation section. This typification of the section will make it possible in the future to simplify the modeling of the properties of bazhenov high-carbon formation and predicting the most prospective areas.
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