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!
id oai:doaj.org-article:e79e9904a5a54834a114d2e453e4f56c
record_format dspace
spelling oai:doaj.org-article:e79e9904a5a54834a114d2e453e4f56c2021-12-02T17:23:49ZThe influence of the brittle-ductile transition zone on aftershock and foreshock occurrence10.1038/s41467-020-16811-72041-1723https://doaj.org/article/e79e9904a5a54834a114d2e453e4f56c2020-06-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-16811-7https://doaj.org/toc/2041-1723Earth 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.Giuseppe PetrilloEugenio LippielloFrançois P. LandesAlberto RossoNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-10 (2020)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Giuseppe Petrillo
Eugenio Lippiello
François P. Landes
Alberto Rosso
The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
description 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.
format article
author Giuseppe Petrillo
Eugenio Lippiello
François P. Landes
Alberto Rosso
author_facet Giuseppe Petrillo
Eugenio Lippiello
François P. Landes
Alberto Rosso
author_sort Giuseppe Petrillo
title The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
title_short The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
title_full The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
title_fullStr The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
title_full_unstemmed The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
title_sort influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
publisher Nature Portfolio
publishDate 2020
url https://doaj.org/article/e79e9904a5a54834a114d2e453e4f56c
work_keys_str_mv AT giuseppepetrillo theinfluenceofthebrittleductiletransitionzoneonaftershockandforeshockoccurrence
AT eugeniolippiello theinfluenceofthebrittleductiletransitionzoneonaftershockandforeshockoccurrence
AT francoisplandes theinfluenceofthebrittleductiletransitionzoneonaftershockandforeshockoccurrence
AT albertorosso theinfluenceofthebrittleductiletransitionzoneonaftershockandforeshockoccurrence
AT giuseppepetrillo influenceofthebrittleductiletransitionzoneonaftershockandforeshockoccurrence
AT eugeniolippiello influenceofthebrittleductiletransitionzoneonaftershockandforeshockoccurrence
AT francoisplandes influenceofthebrittleductiletransitionzoneonaftershockandforeshockoccurrence
AT albertorosso influenceofthebrittleductiletransitionzoneonaftershockandforeshockoccurrence
_version_ 1718381000156774400