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.
Enregistré dans:
Auteurs principaux: | Peter Shebalin, Clément Narteau |
---|---|
Format: | article |
Langue: | EN |
Publié: |
Nature Portfolio
2017
|
Sujets: | |
Accès en ligne: | https://doaj.org/article/57d76c7c169c4292bc1482a20472b05d |
Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|
Documents similaires
-
Forecasting of the first hour aftershocks by means of the perceived magnitude
par: E. Lippiello, et autres
Publié: (2019) -
The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
par: Giuseppe Petrillo, et autres
Publié: (2020) -
Aftershocks are fluid-driven and decay rates controlled by permeability dynamics
par: Stephen A. Miller
Publié: (2020) -
Interevent-time distribution and aftershock frequency in non-stationary induced seismicity
par: Richard A. J. Post, et autres
Publié: (2021) -
Aftershocks of a Mega Earthquake on Occupational Health in Nepal
par: Ajay Kumar Rajbhandari, et autres
Publié: (2015)