Cargando…
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...
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: | |
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 |
Ejemplares similares
-
Machine Learning Predicts the Timing and Shear Stress Evolution of Lab Earthquakes Using Active Seismic Monitoring of Fault Zone Processes
por: Shreedharan, Srisharan, et al.
Publicado: (2021) -
Acoustic Energy Release During the Laboratory Seismic Cycle: Insights on Laboratory Earthquake Precursors and Prediction
por: Bolton, David C., et al.
Publicado: (2020) -
The High‐Frequency Signature of Slow and Fast Laboratory Earthquakes
por: Bolton, David C., et al.
Publicado: (2022) -
Foreshock properties illuminate nucleation processes of slow and fast laboratory earthquakes
por: Bolton, David C., et al.
Publicado: (2023) -
Two end-member earthquake preparations illuminated by foreshock activity on a meter-scale laboratory fault
por: Yamashita, Futoshi, et al.
Publicado: (2021)