Propagation of coupled Rayleigh-gravity waves on the ocean floor
It is shown that the Ocean-Earth crust interface can propagate gravity-sound Rayleigh waves. Dispersion properties ofwaves and flux of energy are derived. It is shown that the waves split into low and fast velocity branches. The fast branch has amultimode structure and has a cutoff in frequency and...
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| Vydáno v: | Geofísica Internacional |
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| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universidad Nacional Autónoma de México
1999
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=56838406 |
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