Monitoring Seismic Velocity Changes Across the San Jacinto Fault Using Train‐Generated Seismic Tremors

Microseismic noise has been used for seismic velocity monitoring. However, such signals are dominated by low‐frequency surface waves that are not ideal for detecting changes associated with small tectonic processes. Here we show that it is possible to extract stable, high‐frequency body waves using...

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Detalles Bibliográficos
Autores principales: Sheng, Y., Mordret, A., Sager, K., Brenguier, F., Boué, P., Rousset, B., Vernon, F., Higueret, Q., Ben‐Zion, Y.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Research Letter
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9786557/
https://www.ncbi.nlm.nih.gov/pubmed/36582260
http://dx.doi.org/10.1029/2022GL098509

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9786557/
https://www.ncbi.nlm.nih.gov/pubmed/36582260
http://dx.doi.org/10.1029/2022GL098509

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