Ambient seafloor noise excited by earthquakes in the Nankai subduction zone

Excitations of seismic background noises are mostly related to fluid disturbances in the atmosphere, ocean and the solid Earth. Earthquakes have not been considered as a stationary excitation source because they occur intermittently. Here we report that acoustic-coupled Rayleigh waves (at 0.7–2.0 Hz...

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Detalles Bibliográficos
Autores principales: Tonegawa, Takashi, Fukao, Yoshio, Takahashi, Tsutomu, Obana, Koichiro, Kodaira, Shuichi, Kaneda, Yoshiyuki
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4317493/
https://www.ncbi.nlm.nih.gov/pubmed/25635384
http://dx.doi.org/10.1038/ncomms7132

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4317493/
https://www.ncbi.nlm.nih.gov/pubmed/25635384
http://dx.doi.org/10.1038/ncomms7132

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