Year: 2025
Pages: 58-72
UDC: 551.734+552.5
Number: 2
Type: scientific article
DOI: 10.31084/2619-0087/2025-2-4
Topic: Lithology, paleogeography
Authors: Sagdeeva, Nuriya S., Frolov, Artem S.
This paper examines the lithofacies features of the Upper Frasnian (Late Devonian) Kolgan Formation in the southwestern part of the East Orenburg Arch based on detailed analysis of several well sections. The studied rocks exhibit an atypical carbonate-terrigenous composition for the Kolgan Formation, characterized by abundant marine fauna fragments and extensive bioturbation traces. A distinct suite of tempestite indicators has been identified within the succession.
Five principal lithotypes have been recognized and grouped into three lithological packages. The well sections demonstrate a gradual transition from terrigenous to carbonate-terrigenous dominated facies. Sediment accumulation occurred during marine tranWression under storm-influenced conditions, showing a facies shift from tidal flat to lower littoral environments.
The study reveals that existing lithofacies models for the Kolgan Formation fail to explain the high lithological variability and carbonate predominance observed in the southwestern EOA. This paper proposes a revised lithofacies model that accounts for the specific features of the carbonate-terrigenous deposits of the Kolgan Formation in the southwestern part of the East Orenburg Arch.
East Orenburg arch uplift, Fransky stage, Kalgan Formation, tempestites, shallow shelf, lithofacial model