Using Ichnofossils to Correlate Oil-Bearing Deposits in the Devonian Clastic Succession (Pashyian and Timanian Horizons) of the South Tatar Arch

This article outlines the results of the first-ever ichnological study of the Middle Devonian clastic succession in the South Tatar Arch. The analysis of the stratigraphic distribution of trace fossils in the boreholes revealed several levels with biogenic structures such as ichnofossils and bioturb...

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Bibliographic Details
Main Author: D. N. Miftakhutdinova
Format: Article
Language:English
Published: Kazan Federal University 2024-01-01
Series:Učënye Zapiski Kazanskogo Universiteta. Seriâ Estestvennye Nauki
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Online Access:https://uzakuesc.elpub.ru/jour/article/view/46
Description
Summary:This article outlines the results of the first-ever ichnological study of the Middle Devonian clastic succession in the South Tatar Arch. The analysis of the stratigraphic distribution of trace fossils in the boreholes revealed several levels with biogenic structures such as ichnofossils and bioturbation, which proved useful for the correlation of the boreholes. The boundary interval of the Pashyian and Timanian Horizons is made up by a succession of three layers: bioturbated siltstones with Spirophyton burrows, limestones, and mudstones with Lingulichnus burrows. The interval can be traced over the entire area of the South Tatar Arch and may serve as an additional marker for the boundary between the horizons.
ISSN:2542-064X
2500-218X