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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Detalles Bibliográficos
Autores principales: Peter Shebalin, Clément Narteau
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
Materias:
Q
Acceso en línea:https://doaj.org/article/57d76c7c169c4292bc1482a20472b05d
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