Sur les ondes T des séismes des Philippines enregistrées à Nhatrang
According to the authors, T waves recorded at Nhatrang from Philippine Islands earthquakes may present 3 important phases: F and G, T. and M. If h is the depth of the earthquake, a and b the land paths of T waves respectively near the epicenter and the station, these phases may be noted as: ph-Sofar-SV sub(b) for F and G; P sub(a)-Sofar-SV sub(b) for T sub(2) and problably S in sediments, for M. Sofar waves velocity in China sea, between Philippine and Vietnam, has been determined as to be: 1.48 ± 0.03km
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| Main Authors: | , |
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| Format: | article biblioteca |
| Language: | French |
| Published: |
1961
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| Subjects: | Earth Sciences, Oceanography, seismic waves, earthquakes, seismic wave propagation, seismic activity at sea, Philippines, Nhatrang, Vietnam, |
| Online Access: | http://hdl.handle.net/1834/35698 |
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| Summary: | According to the authors, T waves recorded at Nhatrang from Philippine Islands earthquakes may present 3 important phases: F and G, T. and M. If h is the depth of the earthquake, a and b the land paths of T waves respectively near the epicenter and the station, these phases may be noted as: ph-Sofar-SV sub(b) for F and G; P sub(a)-Sofar-SV sub(b) for T sub(2) and problably S in sediments, for M. Sofar waves velocity in China sea, between Philippine and Vietnam, has been determined as to be: 1.48 ± 0.03km |
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