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 of waves and flux of energy are derived. It is shown that the waves split into low and fast velocity branches. The fast branch has a multimode structure and has a cutoff in frequency an...

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Bibliographic Details

Published in:	Geofísica Internacional
Main Authors:	Vladimir V. Grimalsky, J. Sánchez-Mondragón, Masashi Hayakawa, Svetlana V. Koshevaya, Gennadiy N. Burlak
Format:	Article
Language:	English
Published:	Universidad Nacional Autónoma de México, Instituto de Geofísica 1999-09-01
Subjects:	Earthquake Rayleigh wave gravity-sound wave
Online Access:	http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/1999/04/burlak.pdf