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Vol 104
Pages:
110-117
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RUS
Article

Organogenic carbonate rocks of the Silurian of central Tuva and conditions of their formation

Authors:
E. V. Vladimirskaya
A. V. Krivobodrova
Date submitted:
1984-08-11
Date accepted:
1984-10-05
Date published:
1985-04-30

Abstract

Carbonate rocks of the Silurian of Tuva are of exclusively organogenic origin. In Central Tuva they form a significant part of the Silurian strata, are the most diverse in structure and origin.

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References

  1. Atlas of textures and structures of sedimentary rocks. Part 2: Carbonate rocks. Moscow, Nedra, 1969. 706 p.
  2. Vladimirskaya E.V. Biostratigraphy of the Chergakian suprahorizon of Tuva. - Journal of Mining Institute, 1978, part 73, vol.2, p. 10-22.
  3. Vladimirskaya E.V., Krivobodrova A.V. Chergak basin of Tuva. - Journal of Mining Institute, 1981, v. 83, p. 3-11.
  4. Vladimirskaya E.V., Chekhovich V.D., Krivobodrova A.V. et al. Silurus of Central Tuva. - Proc. VSEGEI, New Series, 1977, vol. 202, p. 42-53.
  5. Osipova A.I. About classification of carbonate rocks and their genetic interpretation. - In the book: Problems of lithology and geochemistry of sedimentary rocks and ores. Moscow, Nauka, 1975, p. 260-276.
  6. Pylma L. Comparative lithology of Ordovician carbonate rocks of Northern and Middle Baltica. Tallinn, Valgus, 1982. 163 p.
  7. Decisions of the All-Union Meeting on the Development of Unified Stratigraphic Schemes of the Precambrian, Paleozoic and Quaternary System of Middle Siberia 1979. Part 2. Middle and Upper Paleozoic. Novosibirsk, ed. SNIIGGiIMS, 1982. 215 p.
  8. Silurus of the Siberian Platform. New regional and local stratigraphic subdivisions. Novosibirsk, Nauka, 1979. 96 p.
  9. Silurus of Estonia / Edited by D.L. Kal'o. Tallin, Valgus, 1970. 342 p.

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