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Heating, weakening and shear localization in earthquake rupture

Field and borehole observations of active earthquake fault zones show that shear is often localized to principal deforming zones of order 0.1–10 mm width. This paper addresses how frictional heating in rapid slip weakens faults dramatically, relative to their static frictional strength, and promotes...

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Detalhes bibliográficos
Publicado no:Philos Trans A Math Phys Eng Sci
Autor principal: Rice, James R.
Formato: Artigo
Idioma:Inglês
Publicado em: The Royal Society Publishing 2017
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5580449/
https://ncbi.nlm.nih.gov/pubmed/28827427
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2016.0015
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