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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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| Publicado no: | Sci Adv |
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| Main Authors: | , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
American Association for the Advancement of Science
2016
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| Assuntos: | |
| Acesso em linha: | 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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