The evolving interaction of low-frequency earthquakes during transient slip

Observed along the roots of seismogenic faults where the locked interface transitions to a stably sliding one, low-frequency earthquakes (LFEs) primarily occur as event bursts during slow slip. Using an event catalog from Guerrero, Mexico, we employ a statistical analysis to consider the sequence of...

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Detalles Bibliográficos
Autores principales: Frank, William B., Shapiro, Nikolaï M., Husker, Allen L., Kostoglodov, Vladimir, Gusev, Alexander A., Campillo, Michel
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2016
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4846440/
https://www.ncbi.nlm.nih.gov/pubmed/27152345
http://dx.doi.org/10.1126/sciadv.1501616

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4846440/
https://www.ncbi.nlm.nih.gov/pubmed/27152345
http://dx.doi.org/10.1126/sciadv.1501616

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