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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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Pubblicato in:Philos Trans A Math Phys Eng Sci
Autore principale: Rice, James R.
Natura: Artigo
Lingua:Inglês
Pubblicazione: The Royal Society Publishing 2017
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Accesso online: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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