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Recurrent slow slip event likely hastened by the 2011 Tohoku earthquake
Slow slip events (SSEs) are another mode of fault deformation than the fast faulting of regular earthquakes. Such transient episodes have been observed at plate boundaries in a number of subduction zones around the globe. The SSEs near the Boso Peninsula, central Japan, are among the most documented...
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| Main Authors: | , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2012
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3458319/ https://ncbi.nlm.nih.gov/pubmed/22949688 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1202709109 |
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