The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence

Earth surface continues to slip after large earthquakes at a slow velocity for a period of a year or more. In this study, the authors show how such slow slip before and after large earthquakes relates to the interaction of the brittle zone of the fault with the ductile zone at greater depth.

Guardado en:
Detalles Bibliográficos
Autores principales: Giuseppe Petrillo, Eugenio Lippiello, François P. Landes, Alberto Rosso
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2020
Materias:
Q
Acceso en línea:https://doaj.org/article/e79e9904a5a54834a114d2e453e4f56c
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!