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Vol 101
Pages:
3-9
Download volume:
RUS
Article

Seismic boundaries of the consolidated crust of the Baltic Shield

Authors:
I. V. Litvinenko
Date submitted:
1983-09-05
Date accepted:
1983-11-14
Date published:
1984-12-05

Abstract

As is known, the main information on the structure of the consolidated continental crust is currently obtained by means of depth seismic soundings (DSS). According to DSS data, everywhere in the Earth's crust, gentle seismic boundaries are traced.

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References

  1. Eastern part of the Baltic Shield. Geology and deep structure / Edited by K.O.Kratz. L., Nauka, 1975.
  2. Geology and deep structure of the eastern part of the Baltic Shield / Edited by K.O.Kratz. L., Nauka. 1968.
  3. Grachev Yu.N., Litvinenko I.V., Dehnich M.Ya., Nekrasova K.A. Deep seismic sounding on the territory of the Baltic Shield. - In the book: Seismic Investigations, 12th Section of the IGG Program. Moscow, PH of the USSR Academy of Sciences, 1960.
  4. Earth crust of the eastern part of the Baltic Shield / Edited by K.O. Kratz. L., Nauka, 1978.
  5. Kosminskaya I.P. Method of deep seismic sounding of the Earth's crust and upper mantle. M., Nauka, 1968.
  6. Litvinenko I.V. Features of the Earth Crust Structure of the Eastern Part of the Baltic Shield. - In the book: International Geol. congress, 12th session. Reports of Soviet geologists. M., Nedra, 1965.
  7. Litvinenko I.V. Methods of studying by seismic survey of complex structures of the upper part of the consolidated crust of continents. - Journal of Mining Institute, 1971, Vol. 61, Issue 2.
  8. Litvinenko I.V., Melamud M.E. Efficiency of the Reflected Vola Methodology in Reconnaissance-Spatial Study of the Deep Geological Structure of the Pechenga Structure. Journal of Mining Institute, 1976, vol. 89, iss. 2.
  9. Pavlenkova N.I. Wave Fields and Model of the Earth Crust (Continental Part). Kiev, Naukova Dumka, 1973.

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