About macro- and microrelief of the Mohorovičić discontinuity on the Baltic Shield
Abstract
On the Baltic Shield, in its foreign and Soviet parts, to date a large amount of work has been carried out by methods of explosive and conventional seismology, making it possible to determine the base of the consolidated crust — the Mohorovičić discontinuity (M) — in its various areas.
Область исследования:
(Archived) Without section
Funding:
None
References
- Geology and deep structure of the eastern part of the Baltic Shield. L., Nedra, 1968 (in Russian)
- Deep seismic sounding of the Earth's crust in the USSR. L., Gostoptekhizdat, 1962 (in Russian)
- Zavyalov V. D., Stolyarova E. N. Seismic exploration work by the method of mass spatial sounding (MSS). Prikladn. geofizika , 1957, issue 17 (in Russian)
- Puzyrev N. N. Interpretation of Seismic Data by the Method of Reflected Waves. M., Gostoptekhizdat, 1959 (in Russian)
- Riznichenko Yu. V. Spatial problem of interpretation of reflected-wave travel-time curves. Izv. AN SSSR, ser. geofiz. ., 1946, No. 4 (in Russian)
- Penttila E. Crustal structure in Fennoscandia from seismological and gravimetric observations. Annales Academiae scientiarum Fennicae, ser. A III. Geologica-geographica, 110. Helsinki, 1972
- 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
- 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, 1969. Stockholm, 1971
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