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Vol 109
Pages:
60-66
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RUS
Article

Regularities of formation of engineering-geological conditions of glacial shelves and principles of their zoning

Authors:
M. A. Spiridonov
A. E. Rybalko
M. S. Zakharov
N. G. Korvet
Date submitted:
1985-09-17
Date accepted:
1985-11-29
Date published:
1986-09-19

Abstract

Relatively shallow areas of the Barents, White and Baltic Seas due to the commonality of the main stages of their late geological development belong to a single glacial zone of the European glaciation center.

Область исследования:
(Archived) Without section
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References

  1. Varhatov T.L., Izraelyan G.A. Creation of a freshwater reservoir in Onega Bay. - Hydrotechnics and Land Reclamation, 1981, № 12.
  2. Geology of the White Sea / M.A.Spiridonov, N.A.Devdariani, A.V.Kalinin et al. - Soviet Geology, 1980, No. 4.
  3. Grossvald M.G. Glaciation of the Barents Shelf in the Late Pleistocene and Holocene. - Materials of Glaciologic Investigations, 1987, issue 13, No. 1.
  4. Kagan A.A., Solodukhin M.A. Moraine sediments of the North-West of the USSR. M., Nedra, 1976.
  5. Lomtadze V.D. Engineering Geology. Special Engineering Geology. L., Nedra, 1978.
  6. Nevesskiy E.N., Medvedev V.S., Kalinenko V.V. White Sea. Sedimentogenesis and history of development in the Holocene. Moscow, Nauka, 1977.
  7. Prochukhan D.P. Engineering-geological conditions of dam construction on glacial deposits in Karelia and the Kola Peninsula. - In the book: Geology and Dams. M., Energia, 1967.
  8. Rukhina E.V. Lithology of glacial deposits. L., Nedra, 1973.
  9. Yakovleva T.V., Gurevich V.I. Shell sediments of the White Sea Funnel. - Bottom sediments and biocenoses of the Barents and White Seas. Apatity, PH of the Kola Branch of the Academy of Sciences of the USSR, 1974.

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