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Slow slip events in the roots of the San Andreas fault

Episodic tremor and accompanying slow slip are observed at the down-dip edge of subduction seismogenic zones. While tremors are the seismic signature of this phenomenon, they correspond to a small fraction of the moment released; thus, the associated fault slip can be quantified only by geodetic obs...

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Detalles Bibliográficos
Autores principales: Rousset, Baptiste, Bürgmann, Roland, Campillo, Michel
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6374109/
https://www.ncbi.nlm.nih.gov/pubmed/30788438
http://dx.doi.org/10.1126/sciadv.aav3274