The source scaling and seismic productivity of slow slip transients

Slow slip events (SSEs) represent a slow faulting process leading to aseismic strain release often accompanied by seismic tremor or earthquake swarms. The larger SSEs last longer and are often associated with intense and energetic tremor activity, suggesting that aseismic slip controls tremor genesi...

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Detalles Bibliográficos
Autores principales: Passarelli, Luigi, Selvadurai, Paul Antony, Rivalta, Eleonora, Jónsson, Sigurjón
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8336956/
https://www.ncbi.nlm.nih.gov/pubmed/34348899
http://dx.doi.org/10.1126/sciadv.abg9718

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8336956/
https://www.ncbi.nlm.nih.gov/pubmed/34348899
http://dx.doi.org/10.1126/sciadv.abg9718

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