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Variation of Proportionality Between Stress Drop and Slip, With Implications for Megathrust Earthquakes

Abstract Earthquake stress drop Δσ is related to fault slip via Δσ=C⋅μ⋅DLc, where μ, D, and Lc denote shear modulus, average slip, and fault dimension. C is controlled by the system geometry, characterizes the effective stiffness of the system, and is commonly assumed to be a constant near 1. We use...

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Збережено в:
Бібліографічні деталі
Автори: Baoning Wu, Christodoulos Kyriakopoulos, David D. Oglesby, Kenny J. Ryan
Формат: Artigo
Мова:Inglês
Опубліковано: Wiley 2023-02-01
Серія:Geophysical Research Letters
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Онлайн доступ:https://doi.org/10.1029/2022GL100568
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