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Stress-driven fluid flow controls long-term megathrust strength and deep accretionary dynamics
The heterogeneity of frictional strength along the megathrust earthquake zone critically controls plate coupling and long-term subduction dynamics. However, the persistence and distribution of high-friction segments through space and time remain poorly constrained. Here, we show that accretion proce...
| 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/PMC6609719/ https://www.ncbi.nlm.nih.gov/pubmed/31273309 http://dx.doi.org/10.1038/s41598-019-46191-y |