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Slow earthquakes associated with fault healing on a serpentinized plate interface

Slow earthquakes that occur at subduction zones are distinct from regular earthquakes in terms of their slip behavior. We consider this difference to relate to localized hydration reactions at the plate interface that influence the frictional properties. The results of laboratory friction experiment...

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Detalles Bibliográficos
Autores principales: Katayama, Ikuo, Iwata, Mutsumi, Okazaki, Keishi, Hirauchi, Ken-ichi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2013
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3646269/
http://dx.doi.org/10.1038/srep01784

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