The article reflects the experience of studying carbonate deposits of the Osinsky productive horizon (O-1, B1 formation) within several areas located in the central part of the Nepa-Peleduy arch of the Nepa-Botuoba anteclise, which are the main resource base of Surgutneftegas PJSC in the territory of the Republic of Sakha (Yakutia). In the course of the research, a large amount of factual material was studied, including exploration and production data, transit drilling, core studies, the results of interpretation of 3D-seismic data, the analysis of the main indicators of the development of hydrocarbon deposits in the O-1 formation. The first part of the article provides an overview of the published works on the geological structure of the deposits of the Osinsky horizon in the central part of the Nepa-Peleduy arch and their comparison with the data obtained in the process of studying borehole and remote methods of geological and geophysical research. As a result of the analysis of the accumulated data, a unified conceptual model of the geological structure of the Osinsky horizon was developed. A methodologically substantiated algorithm for mapping the paleofacies zones of the O-1 formation is proposed, based on the combined use of correlation results of deposits from the Usolsky regional suite and the analysis of 3D seismic survey data. A refined paleogeographic model of sediment accumulation of the Osinsky horizon in the central part of the Nepsky arch of Eastern Siberia is presented, the structure of the Osinsky horizon in various facies zones is described in detail.
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