Molecular origin of sliding friction and flash heating in rock and heterogeneous materials
Abstract 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 be...
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| Autores principales: | , |
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| Formato: | article |
| Lenguaje: | EN |
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Nature Portfolio
2020
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| Acceso en línea: | https://doaj.org/article/261c801ef3ab42b189248996d4bca926 |
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