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Aftershocks are fluid-driven and decay rates controlled by permeability dynamics
oleh: Stephen A. Miller
Format: | Article |
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Diterbitkan: | Nature Portfolio 2020-11-01 |
Deskripsi
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