Lower phamen of the South Urals
Authors:
Abstract
The classic section of the Lower Phamene is considered to be the section of the central regions of the Russian Platform. In it, the Zadonian and Yeletsky layers with numerous representatives of the Cyrtospirifer archiaci Murch group lie on the Upper Nefranian sediments with theodossia, covered by the Dankov-Lebedian layers with C. lebedianicus Nal.
Область исследования:
(Archived) Without section
Funding:
None
References
- Donanova L. M. Early Carboniferous brachiopods of the Magnitogorsk synclinorium. Cand. dissertation. VSEGEI, 1969.
- Keller B.M. The Paleozoic flysch formation in the Zilair synclinorium in the Southern Urals and similar formations. Proc. IMS AS USSR, Ser. Geol. 104, 1949.
- Perna E. Ya. Paleozoic of the eastern slope of the Urals between Verkhneuralsk and Magnitnaya Station. Proc. Geolkom, vol. XXXI, 1912.
- Smirnova G. A. and Smirnova T. A. Materials to the Paleogeography of the Urals. Essay IV. The Turnean Age. UB AS USSR, Institute of Geology and Geochemistry. Sverdlovsk, 1967.
- Sartenaer P. Senkenberg. Lethaea, Bd. 49, № 5/6, 1968.
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