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Seismic potential of weak, near-surface faults revealed at plate tectonic slip rates
The near-surface areas of major faults commonly contain weak, phyllosilicate minerals, which, based on laboratory friction measurements, are assumed to creep stably. However, it is now known that shallow faults can experience tens of meters of earthquake slip and also host slow and transient slip ev...
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| Pubblicato in: | Sci Adv |
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| Autori principali: | , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
American Association for the Advancement of Science
2017
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5706663/ https://ncbi.nlm.nih.gov/pubmed/29202027 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1701269 |
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