Structural features of terrigenous deposits of the Kolgan strata according to geological modeling data

UDK: 550.834.05:551.31
DOI: 10.24887/0028-2448-2025-4-46-52
Key words: 3D seismic exploration, Kolgan formation, tectonics, Sol-Iletsk arch, Orenburg swell, stratigraphy, paleogeography, Kolgan seismostratigraphic complex, sandstone lens, Devonian, clinoforms, distribution zone, formation conditions, Kolgan-Borisovskaya paleo-depression, geological modeling, depocenter, geological exploration, deposits
Authors: V.N. Kruglov (SamaraNIPIneft LLC, RF, Samara); V.A. Kolesnikov (SamaraNIPIneft LLC, RF, Samara); K.S. Reityukhov (SamaraNIPIneft LLC, RF, Samara); A.P. Lopatin (Orenburgneft JSC, RF, Buzuluk); I.A. Kurashov (Orenburgneft JSC, RF, Buzuluk); S.M. Grigorenko (Rosneft Oil Company, RF, Moscow)

In connection with the recent geological modeling studies, an updated geological model of the Kolgan terrigenous strata of the Upper Devonian in the south of the Orenburg region is presented. The depth-velocity geologic model reveals a number of features of its structure. For the first time it was shown that the boundaries of the Kolgan formation spreading were delineated based on the results of interpretation of the common depth point method (CDPM)-3D seismic depth cube. The presence of the Kolgansko-Borisovsky paleo-trough was clarified and proved. It is noted that all deposits of the Kolgan formation are mainly located in the areas of tectonic faults and have structural-tectonic and lithological-sedimentary nature. The main productive reservoirs are made of terrigenous sandy sediments and have nomination Dkt1 - Dkt3, possibly in some wells there are Dkt4, Dkt5 reservoirs. At present 41 deposits have been discovered at 16 fields. As a result of this work, the zone of Kolgan deposits development within this paleo-fall was established, which is an additional tool for searching for hydrocarbon deposits in Dkt group formations. The boundaries of the Kolgan formation distribution can be clarified not only on the basis of well logging data, but also on the basis of seismic data. Based on the complex of data, the Kolgan strata thicknesses increase in the north and northeast directions from the territory of Zemlyansky license area, therefore, when planning further exploration in the region, attention should be paid to this fact when studying neighboring territories.

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