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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...
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| Udgivet i: | J Geophys Res Solid Earth |
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| Main Authors: | , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
John Wiley and Sons Inc.
2021
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8047899/ https://ncbi.nlm.nih.gov/pubmed/33868888 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1029/2020JB021024 |
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