Cargando…
Dynamic weakening during earthquakes controlled by fluid thermodynamics
Earthquakes result from weakening of faults (transient decrease in friction) during co-seismic slip. Dry faults weaken due to degradation of fault asperities by frictional heating (e.g. flash heating). In the presence of fluids, theoretical models predict faults to weaken by thermal pressurization o...
Autores principales: | Acosta, M., Passelègue, F. X., Schubnel, A., Violay, M. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2018
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6079085/ https://www.ncbi.nlm.nih.gov/pubmed/30082789 http://dx.doi.org/10.1038/s41467-018-05603-9 |
Ejemplares similares
-
Initial effective stress controls the nature of earthquakes
por: Passelègue, François X., et al.
Publicado: (2020) -
Earthquake Nucleation Along Faults With Heterogeneous Weakening Rate
por: Lebihain, Mathias, et al.
Publicado: (2021) -
Fast-moving dislocations trigger flash weakening in carbonate-bearing faults during earthquakes
por: Spagnuolo, Elena, et al.
Publicado: (2015) -
Origin of the Co‐Seismic Variations of Elastic Properties in the Crust: Insight From the Laboratory
por: Paglialunga, F., et al.
Publicado: (2021) -
G: Fracture energy, friction and dissipation in earthquakes
por: Nielsen, S., et al.
Publicado: (2016)