Late Devonian Deltaic System in the East of the Middle Urals

O. Yu. Melnichuk

Abstract


Specific features of facies content and cyclicity of the Upper Devonian Kodinkskaya Suite are considered. In a result, different sedimentary environments are defined: delta front, prodelta, shoreface and offshore. We revealed that sedimentation occurred in conditions of the general marine transgression.

Keywords


facies associations; delta; cyclicity; Upper Devonian; Middle Urals; Kodinkskaya Suite

References


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DOI: http://dx.doi.org/10.17072/psu.geol.17.1.18

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