Arc magma compositions controlled by linked thermal and chemical gradients above the subducting slab

Global arc magmatism is sustained by a continuous fluid flux that is returned to the mantle in subduction zones. Despite considerable advances in simulations of melting processes, models of arc magmatism remain incompletely tested against erupted products. Here, we show that a suite of primitive vol...

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Bibliographic Details
Published in:Geophysical research letters 2013-06, Vol.40 (11), p.2550-2556
Main Authors: Watt, Sebastian F. L., Pyle, David M., Mather, Tamsin A., Naranjo, José A.
Format: Article
Language:English
Subjects:
Arc magma generation
Chemistry
Chile
Electric arc melting
Fluid flow
Fluids
Flux
Magma
Melts
Picrite
Preserves
Primary melt
Primitive magma
Scoria cone
Slabs
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Summary:Global arc magmatism is sustained by a continuous fluid flux that is returned to the mantle in subduction zones. Despite considerable advances in simulations of melting processes, models of arc magmatism remain incompletely tested against erupted products. Here, we show that a suite of primitive volcanic rocks from across the southern Chilean arc preserves the signature of a systematic down‐slab gradient in fluid chemistry. The chemical gradient is consistent with predictions from modeling, geothermometry and experiments. We infer that increasing slab‐surface temperatures cause the sub‐arc slab flux to become less water‐rich and increasingly dominated by hydrous melts over a distance of a few kilometers behind the arc front. This change exerts a first‐order control on magma chemistry, and implies discrete melt‐transport pathways through subduction zones. Our results replicate patterns in other arcs, implying common sub‐arc slab‐surface temperature ranges in thermally‐diverse subduction zones. Key Points Mafic arc rocks preserve a systematic down‐slab magma chemical gradient This reflects increasing dominance of hydrous melts in the slab flux This change, over a few km, is a first‐order control on melt chemistry
ISSN:0094-8276
1944-8007
DOI:10.1002/grl.50513