Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone

In subduction zones, seismic slip at shallow crustal depths can lead to the generation of tsunamis. Large slip displacements during tsunamogenic earthquakes are attributed to the low coseismic shear strength of the fluid-saturated and non-lithified clay-rich fault rocks. However, because of experime...

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Detalles Bibliográficos
Autores principales: Aretusini, S., Meneghini, F., Spagnuolo, E., Harbord, C. W., Di Toro, G.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8087711/
https://www.ncbi.nlm.nih.gov/pubmed/33931641
http://dx.doi.org/10.1038/s41467-021-22805-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8087711/
https://www.ncbi.nlm.nih.gov/pubmed/33931641
http://dx.doi.org/10.1038/s41467-021-22805-w

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