Seismic evidence for flow in the hydrated mantle wedge of the Ryukyu subduction zone

It is widely accepted that water-rich serpentinite domains are commonly present in the mantle above shallow subducting slabs and play key roles in controlling the geochemical cycling and physical properties of subduction zones. Thermal and petrological models show the dominant serpentine mineral is...

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Detalles Bibliográficos
Autores principales: Nagaya, Takayoshi, Walker, Andrew M., Wookey, James, Wallis, Simon R., Ishii, Kazuhiko, Kendall, J. -Michael
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4951697/
https://www.ncbi.nlm.nih.gov/pubmed/27436676
http://dx.doi.org/10.1038/srep29981

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4951697/
https://www.ncbi.nlm.nih.gov/pubmed/27436676
http://dx.doi.org/10.1038/srep29981

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