Subseismic to Seismic Slip in Smectite Clay Nanofoliation

Smectite clays are the main constituent of slipping zones found in subduction zone faults at shallow depth (e.g., <1‐km depth in the Japan Trench) and in the decollements of large landslides (e.g., 1963 landslide, Vajont, Italy). Therefore, deformation processes in smectite clays may control the...

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Detalles Bibliográficos
Autores principales: Aretusini, S., Plümper, O., Spagnuolo, E., Di Toro, G.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6919425/
https://www.ncbi.nlm.nih.gov/pubmed/31894196
http://dx.doi.org/10.1029/2019JB017364

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6919425/
https://www.ncbi.nlm.nih.gov/pubmed/31894196
http://dx.doi.org/10.1029/2019JB017364

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