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Aftershocks are fluid-driven and decay rates controlled by permeability dynamics

One aspect of earthquake physics not adequately addressed is why some earthquakes generate thousands of aftershocks while other earthquakes generate few, if any, aftershocks. It also remains unknown why aftershock rates decay as ~1/time. Here, I show that these two are linked, with a dearth of after...

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Dades bibliogràfiques
Publicat a:Nat Commun
Autor principal: Miller, Stephen A.
Format: Artigo
Idioma:Inglês
Publicat: Nature Publishing Group UK 2020
Matèries:
Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC7666175/
https://ncbi.nlm.nih.gov/pubmed/33188178
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-020-19590-3
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