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Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench
It has been recognized that even weakly coupled subduction zones may cause large interplate earthquakes leading to destructive tsunamis. The Ryukyu Trench is one of the best fields to study this phenomenon, since various slow earthquakes and tsunamis have occurred; yet the fault structure and seismi...
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| Publicado no: | Nat Commun |
|---|---|
| Main Authors: | , , , , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group
2016
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4961848/ https://ncbi.nlm.nih.gov/pubmed/27447546 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms12255 |
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