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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...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5706663/ https://www.ncbi.nlm.nih.gov/pubmed/29202027 http://dx.doi.org/10.1126/sciadv.1701269 |