Mantle hydration along outer-rise faults inferred from serpentinite permeability

Recent geophysical surveys indicate that hydration (serpentinization) of oceanic mantle is related to outer-rise faulting prior to subduction. The serpentinization of oceanic mantle influences the generation of intermediate-depth earthquakes and subduction water flux, thereby promoting arc volcanism...

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Detalles Bibliográficos
Autores principales: Hatakeyama, Kohei, Katayama, Ikuo, Hirauchi, Ken-ichi, Michibayashi, Katsuyoshi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5654952/
https://www.ncbi.nlm.nih.gov/pubmed/29066745
http://dx.doi.org/10.1038/s41598-017-14309-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5654952/
https://www.ncbi.nlm.nih.gov/pubmed/29066745
http://dx.doi.org/10.1038/s41598-017-14309-9

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