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The concept of the formation of the Kama-Kinel depression system from the standpoint of tectonics and sedimentation features in the Late Devonian

Abstract

The origin of the Kama-Kinel system of depressions (KKDS), a system of sub-latitudinal channels that control the position of oil deposits in the Domanik high-carbon formation (DHCF), was considered. The work compares existing hypotheses with data on lithological indicators (tempestites, calciturbidites, spiculites), paleogeographic reconstructions and analogies with Riphean aulacogens. It turned out that the riftogenic factor was secondary. Climate and sedimentary processes came to the fore: storm activity and trade winds. In the shallow basins of the low latitudes of Laurussia, they caused anoxia, accumulation of kerogen, and clinoform filling of depressions. In the axial zones of KKDS, the thickness of the deposits is 30-40 m, which is noticeably lower than the economically justified threshold for multi-stage hydraulic fracturing (about 80 m). Nevertheless, it is precisely to such sections that the new fields put on the balance sheet in 2017-2019. in the Orenburg and Samara regions. The results obtained can be used in the forecast of unconventional oil deposits in high-carbon carbonate-siliceous strata of the VolgaUral province. The formation and evolution of KKDS appears to have been determined by paleohydrodynamics and climate rather than an inherited fault structure.

About the Authors

P. A. Fokin
Lomonosov Moscow State University
Russian Federation

Pavel A. Fokin – PhD in Geological and Mineralogical Sciences, Associate Professor of the Department of Regional Geology and History of the Earth, Faculty of Geology



G. A. Kalmykov
Lomonosov Moscow State University
Russian Federation

Georgy A. Kalmykov – Doctor of Geological and Mineralogical Sciences, Head of the Department of Oil and Gas Sedimentology and Marine Geology, Faculty of Geology



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Fokin P.A., Kalmykov G.A. The concept of the formation of the Kama-Kinel depression system from the standpoint of tectonics and sedimentation features in the Late Devonian. Hard-to-recover reserves. 2026;1(1):28-37. (In Russ.)

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