Head Wave Propagation is a seismic wave propagation phenomenon in which refracted waves travel along an interface between two media with differing seismic velocities, generating energy that radiates upward into the upper medium at the critical angle, thereby enabling the detection of subsurface geological structures in seismic refraction studies.
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Vlastislav Červený, Ravi Ravindra, David P. Hill · American Journal of Physics · 1973 · 306 citations
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University of California San Diego
San Diego, United States
5 h-index
8 publications
439 citations
Scripps Institution of Oceanography
La Jolla, United States
4 h-index
6 publications
295 citations
University of Alberta
Edmonton, Canada
3 h-index
7 publications
84 citations
University of Iowa
Iowa City, United States
3 h-index
11 publications
282 citations
Tel Aviv University
Tel Aviv, Israel
2 h-index
3 publications
66 citations
University of Kassel
Kassel, Germany
2 h-index
6 publications
240 citations
University of Toronto
Toronto, Canada
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3 publications
139 citations
Schlumberger (United States)
Houston, United States
2 h-index
3 publications
488 citations
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- Geophysics
13 publications · 1.4K citations
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- The Journal of the Acoustical Society of America
JASA · 10 publications · 181 citations
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- Geophysical Journal International
GJI · 9 publications · 327 citations
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- Bulletin of the Seismological Society of America
BSSA · 6 publications · 410 citations
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- Journal of Geophysical Research Atmospheres
JGR · 4 publications · 555 citations
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