Lower Famennian of the Southern Urals
Authors:
Abstract
The classic section of the Lower Famennian is considered to be the section of the central regions of the Russian Platform. In it, the Zadonsk and Yelets layers with numerous representatives of the Cyrtospirifer archiaci group lie on the Upper Frasnian sediments with Theodossia, and are covered by the Dankov-Lebedyansk layers with C. lebedianicus.
Область исследования:
(Archived) Without section
Funding:
None
References
- Domanova L. M. Early Carboniferous brachiopods of the Magnitogorsk synclinorium. Avtoref. kand. diss. VSEGEI, 1969. (in Russian)
- Keller B. M. The Paleozoic flysch formation in the Zilair synclinorium in the Southern Urals and similar formations. Tr. IGN AN SSSR, ser. geol. iss. 104, 1949. (in Russian)
- Perna E. Ya. Paleozoic of the eastern slope of the Urals between Verkhneuralsk and Magnitnaya Station. Izv. Geolkoma, vol. XXXI, 1912. (in Russian)
- Smirnova G. A., Smirnova T. A. Materials to the Paleogeography of the Urals. Essay IV. The Tournaisian Age. UF AN SSSR, Institut geologii i geokhimii. Sverdlovsk, 1967. (in Russian)
- Sartenaer P. Senkenberg. Lethaea, Vol. 49, No. 5/6, 1968. (in Russian)
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