Accretionary prism collapse: a new hypothesis on the source of the 1771 giant tsunami in the Ryukyu Arc, SW Japan

The giant 1771 Yaeyama tsunami occurred in the southwestern part of the Ryukyu Arc, a region on an obliquely subducting plate boundary, which shows no direct evidence of inter-plate coupling. Studies of tsunami boulders and deposits suggest that the recurrence interval of comparably giant tsunamis i...

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Detalles Bibliográficos
Autores principales: Okamura, Yukinobu, Nishizawa, Azusa, Fujii, Yushiro, Yanagisawa, Hideaki
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6134009/
https://www.ncbi.nlm.nih.gov/pubmed/30206405
http://dx.doi.org/10.1038/s41598-018-31956-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6134009/
https://www.ncbi.nlm.nih.gov/pubmed/30206405
http://dx.doi.org/10.1038/s41598-018-31956-8

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