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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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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: Nagaya, Takayoshi, Walker, Andrew M., Wookey, James, Wallis, Simon R., Ishii, Kazuhiko, Kendall, J. -Michael
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group 2016
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC4951697/
https://ncbi.nlm.nih.gov/pubmed/27436676
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep29981
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