Large slip, long duration, and moderate shaking of the Nicaragua 1992 tsunami earthquake caused by low near-trench rock rigidity

Large earthquake ruptures propagating up to areas close to subduction trenches are infrequent, but when they occur, they heavily displace the ocean seafloor originating destructive tsunamis. The current paradigm is that the large seafloor deformation is caused by local factors reducing friction and...

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Detalles Bibliográficos
Autores principales: Sallarès, Valentí, Prada, Manel, Riquelme, Sebastián, Meléndez, Adrià, Calahorrano, Alcinoe, Grevemeyer, Ingo, Ranero, César R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8346212/
https://www.ncbi.nlm.nih.gov/pubmed/34362735
http://dx.doi.org/10.1126/sciadv.abg8659

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8346212/
https://www.ncbi.nlm.nih.gov/pubmed/34362735
http://dx.doi.org/10.1126/sciadv.abg8659

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