Frequency‐Magnitude Statistics of Laboratory Foreshocks Vary With Shear Velocity, Fault Slip Rate, and Shear Stress

Understanding the temporal evolution of foreshocks and their relation to earthquake nucleation is important for earthquake early warning systems, earthquake hazard assessment, and earthquake physics. Laboratory experiments on intact rock and rough fractures have demonstrated that the number and size...

Descripción completa

Detalles Bibliográficos
Autores principales: Bolton, David C., Shreedharan, Srisharan, Rivière, Jacques, Marone, Chris
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2021
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9286047/
https://www.ncbi.nlm.nih.gov/pubmed/35865108
http://dx.doi.org/10.1029/2021JB022175

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9286047/
https://www.ncbi.nlm.nih.gov/pubmed/35865108
http://dx.doi.org/10.1029/2021JB022175

Ejemplares similares