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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...
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| Publicado en: | Nat Commun |
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| Main Authors: | , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Nature Publishing Group UK
2018
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| Assuntos: | |
| Acceso en liña: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6079085/ https://ncbi.nlm.nih.gov/pubmed/30082789 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-05603-9 |
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