Surface faulting earthquake clustering controlled by fault and shear-zone interactions

Surface faulting earthquakes are known to cluster in time from historical and palaeoseismic studies, but the mechanism(s) responsible for clustering, such as fault interaction, strain-storage, and evolving dynamic topography, are poorly quantified, and hence not well understood. We present a quantif...

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Detalles Bibliográficos
Autores principales: Mildon, Zoë K., Roberts, Gerald P., Faure Walker, Joanna P., Beck, Joakim, Papanikolaou, Ioannis, Michetti, Alessandro M., Toda, Shinji, Iezzi, Francesco, Campbell, Lucy, McCaffrey, Kenneth J. W., Shanks, Richard, Sgambato, Claudia, Robertson, Jennifer, Meschis, Marco, Vittori, Eutizio
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9681762/
https://www.ncbi.nlm.nih.gov/pubmed/36414645
http://dx.doi.org/10.1038/s41467-022-34821-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9681762/
https://www.ncbi.nlm.nih.gov/pubmed/36414645
http://dx.doi.org/10.1038/s41467-022-34821-5

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