Seismic evidence for megathrust fault-valve behavior during episodic tremor and slip

Fault slip behavior during episodic tremor and slow slip (ETS) events, which occur at the deep extension of subduction zone megathrust faults, is believed to be related to cyclic fluid processes that necessitate fluctuations in pore-fluid pressures. In most subduction zones, a layer of anomalously l...

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Detalles Bibliográficos
Autores principales: Gosselin, Jeremy M., Audet, Pascal, Estève, Clément, McLellan, Morgan, Mosher, Stephen G., Schaeffer, Andrew J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2020
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6976297/
https://www.ncbi.nlm.nih.gov/pubmed/32010787
http://dx.doi.org/10.1126/sciadv.aay5174

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6976297/
https://www.ncbi.nlm.nih.gov/pubmed/32010787
http://dx.doi.org/10.1126/sciadv.aay5174

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