Rock friction and its implications for earthquake prediction examined via models of Parkfield earthquakes.
The friction of rocks in the laboratory is a function of time, velocity of sliding, and displacement. Although the processes responsible for these dependencies are unknown, constitutive equations have been developed that do a reasonable job of describing the laboratory behavior. These constitutive l...
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| Vydáno v: | Proc Natl Acad Sci U S A |
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| Hlavní autor: | |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
1996
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC39440/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/11607668/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.93.9.3803 |
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