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Vol 63 Iss. 2
Pages:
53-59
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RUS
Article

New data on the age of the Kosva horizon of the Lower Carboniferous on the basis of ostracods

Authors:
I. D. Tkacheva
Date submitted:
1971-08-11
Date accepted:
1971-10-04
Date published:
1972-02-01

Abstract

The tier affiliation of the Kosva horizon is debatable. The existing points of view are based on different interpretation of geological and faunistic data. Ostracods of the Kosvinsky horizon were studied in two sections of the western slope of the Urals - “Shirokovsky” (Middle Urals, Kizelovsky district) and “Usuili” (Zilim River basin).

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References

  1. Gorsky I. I. Geological sketch of the Kizelovsky district. Coll. Carboniferous sediments of the western slope of the Urals. PH VGRO, 1932.
  2. Malakhova N. I. Turnean Stage of the Northern and Middle Urals. Proc. GTI UFAN USSR, vol. 38, 1959.
  3. Nalivkin D. V. Sterlitamak crossing of the Southern Urals. Intern. Geol. Congr., XVII session. Perm Excursion. Southern Route, M., ONTI, 1937.
  4. Nalivkin D. V. The boundary of the Turnean and Visean stages in the Urals and the methodology of its establishment. Mat. All-Russian Geological Institute, vol. 5, 1948.
  5. Tebenkov V. P. New Data on Stratigraphy of the Turnean Deposits of the Kizelov Area. Sov. Geology, vol. 9, No. 1, 1939.
  6. Chizhova V. A. Ostracods of the Kizelov horizon of the Saratov-Volgograd Volga Region. Proc. VNII, vol. 14, 1958.
  7. Chizhova V. A. Age correlation of the Rakov and Lower Malinov deposits of the Kamsko-Kinelskaya Depression according to ostracods. Proc. VNII, vol. 30, 1960.
  8. Shcherbakov O. A. et al. To the stratigraphy of the boundary layers of the Turnean and Visean stages in the Middle Urals. RAN USSR, vol. 158, No. 1, 1964.
  9. Jones T. et Kirkhy J. J. Geol. Soc. (Britain), vol. 35, 1879.
  10. Kummerov E. H. Abhandl. Prenss. Geol. Landesanst., N. F. Hft. 194, 1939.

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