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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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| Pubblicato in: | Sci Rep |
|---|---|
| Autori principali: | , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group
2016
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| Soggetti: | |
| Accesso online: | 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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