Kinematic Afterslip Patterns
Abstract Non‐inertial afterslip has been inferred to occur following large earthquakes. An explanation for this slow slip phenomenon is that coseismically generated stresses induce sliding on parts of a fault surface with velocity‐strengthening frictional properties. Here we develop an alternative m...
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| Autor Principal: | |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Wiley
2024-01-01
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| Series: | Geophysical Research Letters |
| Acceso en liña: | https://doi.org/10.1029/2023GL105797 |
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