The Behaviour of Halogens (F, Cl, Br, I) and Other Fluid-Mobile Elements in Subduction Zones
The high abundance of fluid-mobile elements (FMEs) in arc magmas relative to the mantle attests to their recycling in subduction zones. Aqueous fluids released from the subducting slab transport these elements to the overlying mantle wedge for arc magma generation. However, some FME may be retained...
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Format: | Others |
Language: | en |
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Université d'Ottawa / University of Ottawa
2019
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Online Access: | http://hdl.handle.net/10393/39261 http://dx.doi.org/10.20381/ruor-23508 |