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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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Bibliografiske detaljer
Udgivet i:Nat Commun
Main Authors: Acosta, M., Passelègue, F. X., Schubnel, A., Violay, M.
Format: Artigo
Sprog:Inglês
Udgivet: Nature Publishing Group UK 2018
Fag:
Online adgang: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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