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Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake
The deformation transient following large subduction zone earthquakes is thought to originate from the interaction of viscoelastic flow in the asthenospheric mantle and slip on the megathrust that are both accelerated by the sudden coseismic stress change. Here, we show that combining insight from l...
| Autores principales: | , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6435688/ https://www.ncbi.nlm.nih.gov/pubmed/30914636 http://dx.doi.org/10.1038/s41467-019-08984-7 |