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Across‐Fault Velocity Gradients and Slip Behavior of the San Andreas Fault Near Parkfield
A long‐lasting question in earthquake physics is why slip on faults occurs as creep or dynamic rupture. We compute passive measurements of the seismic P wave velocity gradient across the San Andreas Fault near Parkfield, where this transition of slip mode occurs at a scale of a few kilometers. Unbia...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
John Wiley and Sons Inc.
2020
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7374945/ https://www.ncbi.nlm.nih.gov/pubmed/32713971 http://dx.doi.org/10.1029/2019GL084480 |