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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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Autor principal: Tullis, T E
Format: Artigo
Idioma:Inglês
Publicat: 1996
Matèries:
Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC39440/
https://ncbi.nlm.nih.gov/pubmed/11607668
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