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High time-resolved studies of stick–slip show similar dilatancy to fast and slow earthquakes
Fast and slow earthquakes are two modes of energy release by the slip in tectonic fault rupture. Although fast and slow slips were observed in the laboratory stick–slip experiments, due to the sampling rate limitation, the details of the fault thickness variation were poorly understood. Especially,...
| Autores principales: | , , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
National Academy of Sciences
2023
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10666130/ https://www.ncbi.nlm.nih.gov/pubmed/37967222 http://dx.doi.org/10.1073/pnas.2305134120 |