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Vol 66 Iss. 2
Pages:
3-12
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RUS
Article

About macro- and microrelief of the Mohorovičić discontinuity on the Baltic Shield

Authors:
I. V. Litvinenko
L. N. Platonenkova
N. I. Suvorova
Date submitted:
1973-08-17
Date accepted:
1973-10-24
Date published:
1974-02-01

Abstract

On the Baltic Shield, in foreign and Soviet parts of it, to date, a large amount of work has been carried out by methods of explosive and conventional seismology, allowing to determine the sole of the consolidated crust - the Mohorovičić discontinuity (M) - in its various areas.

Область исследования:
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References

  1. Geology and deep structure of the eastern part of the Baltic Shield. L., Nedra. 1968.
  2. Deep seismic sounding of the Earth's crust in the USSR. L., Gostoptekhizdat, 1962.
  3. Zavyalov V.D., Stolyarova E. N. Seismic exploration works by the method of mass spatial sounding (MSS). applied geophysics, 1957, issue 17.
  4. Puzyrev N. N. Interpretation of Seismic Data by the Method of Reflected Waves. Moscow, Gostoptekhizdat, 1959.
  5. Riznichenko Yu. V. Spatial Problem of Interpretation of Reflected Wave Godographs. - Proc. of the AS USSR, Ser. Geophys., 1946, No. 4.
  6. Penttila E. Crustal structure in Fennoscandia from seismological and gravimetric observations.- Annales Academiae scientiarum Fennicae, ser. A III. Geologica-geographica, 110. Helsinki, 1972.
  7. Sellevoll M. A. Report from the Sub-Commission on explosion work in Northern Europe. Prepared for the European Seismological, meeting in Luxemburg, 21-29 Sept. 1970. Bergen, 1970.
  8. Vogel A. Deep seismic sounding in Northern Europe. Proceedings of the colloquium on deep seismic sounding in Northern Europe held in Uppsala on december 1, and 2, 1,969. Stockholm, 1971.

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