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Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake
Modeling of postseismic deformation following great earthquakes has revealed the viscous structure of the mantle and the frictional properties of the fault interface. However, for giant megathrust events, viscoelastic flow and afterslip mechanically interplay with each other during the postseismic p...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6760927/ https://www.ncbi.nlm.nih.gov/pubmed/31579819 http://dx.doi.org/10.1126/sciadv.aaw1164 |