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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...
שמור ב:
| הוצא לאור ב: | Nat Commun |
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| Main Authors: | , , , |
| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
Nature Publishing Group UK
2018
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| נושאים: | |
| גישה מקוונת: | 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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