Depth dependent stress revealed by aftershocks
Aftershocks are earthquakes triggered in the near field by the dynamic rupture of larger earthquake events. Here, the authors show along the San Andreas fault system that the early aftershock decay rate can be used to infer the variations of stress with depth.
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| Autores principales: | , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2017
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/57d76c7c169c4292bc1482a20472b05d |
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| Sumario: | Aftershocks are earthquakes triggered in the near field by the dynamic rupture of larger earthquake events. Here, the authors show along the San Andreas fault system that the early aftershock decay rate can be used to infer the variations of stress with depth. |
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