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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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| Publicado en: | J Geophys Res Solid Earth |
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| Main Authors: | , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
John Wiley and Sons Inc.
2019
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| Assuntos: | |
| Acceso en liña: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6919425/ https://ncbi.nlm.nih.gov/pubmed/31894196 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1029/2019JB017364 |
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