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Bridging time scales of faulting: From coseismic to postseismic slip of the M(w) 6.0 2014 South Napa, California earthquake
Transient fault slip spans time scales from tens of seconds of earthquake rupture to years of aseismic afterslip. So far, seismic and geodetic recordings of these two phenomena have primarily been studied separately and mostly with a focus on kinematic aspects, which limits our physical understandin...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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American Association for the Advancement of Science
2022
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9506709/ https://www.ncbi.nlm.nih.gov/pubmed/36149958 http://dx.doi.org/10.1126/sciadv.abq2536 |