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Molecular origin of sliding friction and flash heating in rock and heterogeneous materials
It is generally believed that earthquakes occur when faults weaken with increasing slip rates. An important factor contributing to this phenomenon is the faults’ dynamic friction, which may be reduced during earthquakes with high slip rates, a process known as slip-rate weakening. It has been hypoth...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2020
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7747623/ https://www.ncbi.nlm.nih.gov/pubmed/33335303 http://dx.doi.org/10.1038/s41598-020-79383-y |