Areas prone to slow slip events impede earthquake rupture propagation and promote afterslip

At subduction zones, transient aseismic slip occurs either as afterslip following a large earthquake or as episodic slow slip events during the interseismic period. Afterslip and slow slip events are usually considered as distinct processes occurring on separate fault areas governed by different fri...

Descripción completa

Detalles Bibliográficos
Autores principales: Rolandone, Frederique, Nocquet, Jean-Mathieu, Mothes, Patricia A., Jarrin, Paul, Vallée, Martin, Cubas, Nadaya, Hernandez, Stephen, Plain, Morgan, Vaca, Sandro, Font, Yvonne
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2018
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5796792/
https://www.ncbi.nlm.nih.gov/pubmed/29404404
http://dx.doi.org/10.1126/sciadv.aao6596

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5796792/
https://www.ncbi.nlm.nih.gov/pubmed/29404404
http://dx.doi.org/10.1126/sciadv.aao6596

Ejemplares similares