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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...

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Publicat a:Sci Rep
Autors principals: Menant, Armel, Angiboust, Samuel, Gerya, Taras
Format: Artigo
Idioma:Inglês
Publicat: Nature Publishing Group UK 2019
Matèries:
Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC6609719/
https://ncbi.nlm.nih.gov/pubmed/31273309
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-46191-y
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