Summary
After a structural description of the shape of the Mohorovičić discontinuity as obtained in Central Europe by DSS, a geophysical synthesis is given for the territory of Czechoslovakia under the use of gravimetric, seismologic, geomagnetic, magnetotelluric, geothermic and geodetic data. Particular attention is paid to the contact zone between the Bohemian Massif and the Carpathians.
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References
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Zátopek, A., Beránek, B. Geophysical synthesis and crustal structure in central Europe. Stud Geophys Geod 19, 121–133 (1975). https://doi.org/10.1007/BF01635420
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DOI: https://doi.org/10.1007/BF01635420