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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Veröffentlicht in:Sci Adv
Hauptverfasser: Frank, William B., Shapiro, Nikolaï M., Husker, Allen L., Kostoglodov, Vladimir, Gusev, Alexander A., Campillo, Michel
Format: Artigo
Sprache:Inglês
Veröffentlicht: American Association for the Advancement of Science 2016
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Research Articles
Online Zugang:https://ncbi.nlm.nih.gov/pmc/articles/PMC4846440/
https://ncbi.nlm.nih.gov/pubmed/27152345
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1501616
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