Llandovery conodonts from the outcrop 229 of the River Kozhym (Western slope of Subpolar Ural)
https://doi.org/10.52349/0869-7892_2022_91_45-51
Abstract
As a result of recognire conodont studies, the presence of deposits of two local and one regional conodont zones was established in the outcrop of 229 of the River Kozhym, which made it possible to the regional stratigraphic units – Lolashor, Filipp’’el’ and Marshrutnyj regional stages, previously identified in the outcrop mainly by lithological features.
About the Author
L. V. Sokolova
Institute of Geology of Komi Science Centre of the Ural Branch of the Russian Academy of Sciences – a separate
subdivision of the FRC Komi SC UB RAS (IG FRC Komi SC UB RAS)
Russian Federation
Russian Federation
Sokolova Lyubov Vyacheslavovna – Candidate of Geological and Mineralogical Sciences, Researcher at the Laboratory of Stratigraphy
54 Ul. Pervomayskaya, Syktyvkar, Komi Republic, 167982.
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Review
For citations:
Sokolova L.V. Llandovery conodonts from the outcrop 229 of the River Kozhym (Western slope of Subpolar Ural). Regional Geology and Metallogeny. 2022;(91):45-51. (In Russ.) https://doi.org/10.52349/0869-7892_2022_91_45-51
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