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Microphysical Modeling of Carbonate Fault Friction at Slip Rates Spanning the Full Seismic Cycle
Laboratory studies suggest that seismogenic rupture on faults in carbonate terrains can be explained by a transition from high friction, at low sliding velocities (V), to low friction due to rapid dynamic weakening as seismic slip velocities are approached. However, consensus on the controlling phys...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
John Wiley and Sons Inc.
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8047899/ https://www.ncbi.nlm.nih.gov/pubmed/33868888 http://dx.doi.org/10.1029/2020JB021024 |