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

In this study, the authors propose that a fluid rich environment is necessary to generate long-lasting aftershock sequences. Based on this premise, the study presents a theory for modeling fluid-driven earthquake sequences

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Détails bibliographiques
Auteur principal: Stephen A. Miller
Format: article
Langue:EN
Publié: Nature Portfolio 2020
Sujets:
Q
Accès en ligne:https://doaj.org/article/e97e6ec5075a455cb047d44d37e51b0b
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Description
Résumé:In this study, the authors propose that a fluid rich environment is necessary to generate long-lasting aftershock sequences. Based on this premise, the study presents a theory for modeling fluid-driven earthquake sequences