Summary
The space (time) delay of transmitted waves in the vicinity of the interface beyond the critical point is investigated on two-dimensional seismic models of a low velocity channel; results of laboratory experiments are compared with the conclusions of the theory. The effect of the time delay in field measurements is demonstrated by means of two typical geological formations.
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Dresen, L., Freystätter, S., Kozák, J. et al. Transmitted waves in the vicinity of the interface beyond the critical point. Stud Geophys Geod 21, 137–142 (1977). https://doi.org/10.1007/BF01634824
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DOI: https://doi.org/10.1007/BF01634824