Clock advance and magnitude limitation through fault interaction: the case of the 2016 central Italy earthquake sequence
Abstract Faults communicate with each other. Strong earthquakes perturb stress over large volumes modifying the load on nearby faults and their resistance to slip. The causative fault induces permanent or transient perturbations that can change the time to the next seismic rupture with respect to th...
Guardado en:
Autores principales: | Nicola Alessandro Pino, Vincenzo Convertito, Raul Madariaga |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2019
|
Materias: | |
Acceso en línea: | https://doaj.org/article/88f1e6a4ab5d47508b5877f398e17e15 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Near-field fault slip of the 2016 Vettore Mw 6.6 earthquake (Central Italy) measured using low-cost GNSS
por: Maxwell W. Wilkinson, et al.
Publicado: (2017) -
Coincident locations of rupture nucleation during the 2019 Le Teil earthquake, France and maximum stress change from local cement quarrying
por: Vincenzo De Novellis, et al.
Publicado: (2020) -
Forecasting the magnitude of the largest expected earthquake
por: Robert Shcherbakov, et al.
Publicado: (2019) -
Fault valving and pore pressure evolution in simulations of earthquake sequences and aseismic slip
por: Weiqiang Zhu, et al.
Publicado: (2020) -
Fault reactivation and earthquakes with magnitudes of up to Mw4.7 induced by shale-gas hydraulic fracturing in Sichuan Basin, China
por: Xinglin Lei, et al.
Publicado: (2017)