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
Guardado en:
Autor principal: | Stephen A. Miller |
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Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2020
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Materias: | |
Acceso en línea: | https://doaj.org/article/e97e6ec5075a455cb047d44d37e51b0b |
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