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Slow-slip events in semi-brittle serpentinite fault zones
Slow-slip events are earthquake-like events only with much lower slip rates. While peak coseismic velocities can reach tens of meters per second, slow-slip is on the order of 10(−7±2) m/s and may last for days to weeks. Under the rate-and-state model of fault friction, slow-slip is produced only whe...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2018
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5906616/ https://www.ncbi.nlm.nih.gov/pubmed/29670246 http://dx.doi.org/10.1038/s41598-018-24637-z |