Cargando…
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...
| Autores principales: | , , , , , , , , , |
|---|---|
| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2018
|
| Materias: | |
| 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 |