Ładuje się......
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...
Zapisane w:
| 1. autor: | |
|---|---|
| Format: | Artigo |
| Język: | Inglês |
| Wydane: |
1996
|
| Hasła przedmiotowe: | |
| Dostęp online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC39440/ https://ncbi.nlm.nih.gov/pubmed/11607668 |
| Etykiety: |
Dodaj etykietę
Nie ma etykietki, Dołącz pierwszą etykiete!
|