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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...
Autores principales: | Sheng, Y., Mordret, A., Sager, K., Brenguier, F., Boué, P., Rousset, B., Vernon, F., Higueret, Q., Ben‐Zion, Y. |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
John Wiley and Sons Inc.
2022
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Materias: | |
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 |
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