Propagation of coupled Rayleigh-gravity waves on the ocean floor

Gennadiy N. Burlak; Svetlana V. Koshevaya; Masashi Hayakawa; J. Sánchez-Mondragón; Vladimir V. Grimalsky

doi:10.22201/igeof.00167169p.1999.38.4.508

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Publicado: oct 1, 1999

DOI: https://doi.org/10.22201/igeof.00167169p.1999.38.4.508

Palabras clave:

Sismo, onda Rayleigh, onda de gravedad-acústica

Gennadiy N. Burlak

Centre for Research on Engineering and Applied Sciences, Autonomous State University of Morelos, Cuernavaca, Mor., México

Svetlana V. Koshevaya

Centre for Research on Engineering and Applied Sciences, Autonomous State University of Morelos, Cuernavaca, Mor., México ; INAOE, Puebla, México

Masashi Hayakawa

The University of Electro-Communication, Chofu, Tokyo, Japan

J. Sánchez-Mondragón

Centre for Research on Engineering and Applied Sciences, Autonomous State University of Morelos, Cuernavaca, Mor., México

Vladimir V. Grimalsky

Centre for Research on Engineering and Applied Sciences, Autonomous State University of Morelos, Cuernavaca, Mor., México ; Space Research Institute NASU-NSAU, Kiev, Ukraine

Resumen

El fondo del mar puede propagar ondas acopladas de gravedad, acústicas y de Rayleigh. Se presentan expresiones para la dispersión y el flujo de energía, y se demustra que las ondas se dividen en dos ramas. La rama de lata velocidad tiene estructura multimodal y un corte de alta frecuencia.

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Editor & editorial board: profiles
Academic society: Geofísica Internacional
Editora:: Universidad Nacional Autónoma de México. Instituto de Geofísica

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Cómo citar

Burlak, G. N., Koshevaya, S. V., Hayakawa, M., Sánchez-Mondragón, J., & Grimalsky, V. V. (1999). Propagation of coupled Rayleigh-gravity waves on the ocean floor. Geofísica Internacional, 38(4), 261–268. https://doi.org/10.22201/igeof.00167169p.1999.38.4.508