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Daily measurement of slow slip from low-frequency earthquakes is consistent with ordinary earthquake scaling
Slow slip transients on faults can last from seconds to months and stitch together the earthquake cycle. However, no single geophysical instrument is able to observe the full range of slow slip because of bandwidth limitations. Here, we connect seismic and geodetic data from the Mexican subduction z...
Guardado en:
| Publicado en: | Sci Adv |
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| Autores principales: | , |
| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
American Association for the Advancement of Science
2019
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| Materias: | |
| Acceso en línea: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6774729/ https://ncbi.nlm.nih.gov/pubmed/31616786 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aaw9386 |
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