Belogorsky (Tastubsky) horizon of the Sakmarian Stage of the western Urals
Abstract
For many years, the stratigraphic scheme of the Permian deposits of the Urals has been based on the scheme of D.M. Rauser-Chernousova [1940]. It was developed in accordance with the distribution of individual foraminifera complexes along the section. Many of the horizons identified by D. M. Rauser-Chernousova retained their name and were adopted in the Unified Scheme of Permian sediments of the Urals in 1962, and their sections are considered stratotypic.
Область исследования:
(Archived) Without section
References
- Nalivkin V. D. Stratigraphy and tectonics of the Ufa Plateau and the Yurezano-Sylvenskaya Depression. Proc. VNIGRI, new ser. vol. 46, 1949.
- Rauser-Chernousova D.M. Stratigraphy of the Upper Carboniferous and Artinskian Stage of the Western Slope of the Urals and Materials for the Fauna of Fusulinids. Proc. IGN AS USSR, Geol. ser., vol. 7, 1940.
- Chernyshev F. N. General Geological Map of Russia. Sheet 139. Proc. Geol. com., vol. III, iss. 4, 1889.