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...

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Detalles Bibliográficos
Autores principales: Frank, William B., Brodsky, Emily E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6774729/
https://www.ncbi.nlm.nih.gov/pubmed/31616786
http://dx.doi.org/10.1126/sciadv.aaw9386

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6774729/
https://www.ncbi.nlm.nih.gov/pubmed/31616786
http://dx.doi.org/10.1126/sciadv.aaw9386

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