About macro- and microrelief of the Mohorovičić discontinuity on the Baltic Shield
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:
(Archived) Without section
References
- Geology and deep structure of the eastern part of the Baltic Shield. L., Nedra. 1968.
- Deep seismic sounding of the Earth's crust in the USSR. L., Gostoptekhizdat, 1962.
- Zavyalov V.D., Stolyarova E. N. Seismic exploration works by the method of mass spatial sounding (MSS). applied geophysics, 1957, issue 17.
- Puzyrev N. N. Interpretation of Seismic Data by the Method of Reflected Waves. Moscow, Gostoptekhizdat, 1959.
- Riznichenko Yu. V. Spatial Problem of Interpretation of Reflected Wave Godographs. - Proc. of the AS USSR, Ser. Geophys., 1946, No. 4.
- 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, 1,969. Stockholm, 1971.
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