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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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| Pubblicato in: | Nat Commun |
|---|---|
| Autori principali: | , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group UK
2018
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| Soggetti: | |
| Accesso online: | 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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