Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone

Laboratory experiments reproducing earthquake slip in non cohesive fault rocks under fluid pressurised conditions are challenging. Thanks to these experiments, the authors show that earthquake slip occurring in tsunamigenic subduction zone faults is controlled by dilatancy and pressurisation process...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	S. Aretusini, F. Meneghini, E. Spagnuolo, C. W. Harbord, G. Di Toro
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/86758d62731a442b84d67a3d77cb7ca6
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:86758d62731a442b84d67a3d77cb7ca6
record_format	dspace
spelling	oai:doaj.org-article:86758d62731a442b84d67a3d77cb7ca62021-12-02T17:15:32ZFluid pressurisation and earthquake propagation in the Hikurangi subduction zone10.1038/s41467-021-22805-w2041-1723https://doaj.org/article/86758d62731a442b84d67a3d77cb7ca62021-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-22805-whttps://doaj.org/toc/2041-1723Laboratory experiments reproducing earthquake slip in non cohesive fault rocks under fluid pressurised conditions are challenging. Thanks to these experiments, the authors show that earthquake slip occurring in tsunamigenic subduction zone faults is controlled by dilatancy and pressurisation processes.S. AretusiniF. MeneghiniE. SpagnuoloC. W. HarbordG. Di ToroNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-8 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q S. Aretusini F. Meneghini E. Spagnuolo C. W. Harbord G. Di Toro Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone
description	Laboratory experiments reproducing earthquake slip in non cohesive fault rocks under fluid pressurised conditions are challenging. Thanks to these experiments, the authors show that earthquake slip occurring in tsunamigenic subduction zone faults is controlled by dilatancy and pressurisation processes.
format	article
author	S. Aretusini F. Meneghini E. Spagnuolo C. W. Harbord G. Di Toro
author_facet	S. Aretusini F. Meneghini E. Spagnuolo C. W. Harbord G. Di Toro
author_sort	S. Aretusini
title	Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone
title_short	Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone
title_full	Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone
title_fullStr	Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone
title_full_unstemmed	Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone
title_sort	fluid pressurisation and earthquake propagation in the hikurangi subduction zone
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/86758d62731a442b84d67a3d77cb7ca6
work_keys_str_mv	AT saretusini fluidpressurisationandearthquakepropagationinthehikurangisubductionzone AT fmeneghini fluidpressurisationandearthquakepropagationinthehikurangisubductionzone AT espagnuolo fluidpressurisationandearthquakepropagationinthehikurangisubductionzone AT cwharbord fluidpressurisationandearthquakepropagationinthehikurangisubductionzone AT gditoro fluidpressurisationandearthquakepropagationinthehikurangisubductionzone
_version_	1718381269055700992

Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone

Ejemplares similares