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Transient and Steady‐State Friction in Non‐Isobaric Conditions

Abstract The frictional properties of faults control the initiation and propagation of earthquakes and the associated hazards. Although the ambient temperature and instantaneous slip velocity controls on friction in isobaric conditions are increasingly well understood, the role of normal stress on s...

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Autor principal: Sylvain Barbot
Format: Artigo
Idioma:Inglês
Publicat: Wiley 2024-02-01
Col·lecció:Geochemistry, Geophysics, Geosystems
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Accés en línia:https://doi.org/10.1029/2023GC011279
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