The redox budget of subduction zones

KA Evans - Earth-Science Reviews, 2012 - Elsevier
Elements that can occur in more than one valence state, such as Fe, C and S, play an
important role in Earth's systems at all levels, and can drive planetary evolution as they cycle …

Brines at high pressure and temperature: thermodynamic, petrologic and geochemical effects

CE Manning, LY Aranovich - Precambrian Research, 2014 - Elsevier
A number of observations point to the participation of brines in high-grade metamorphic
processes. These include findings of alkali and alkaline-earth halides as daughter crystals in …

Deserpentinization in subduction zones as a source of oxidation in arcs: A reality check

KA Evans, BR Frost - Journal of Petrology, 2020 - ieeexplore.ieee.org
Previous studies have concluded that dehydration of serpentinites in subduction zones
produces oxidizing fluids that are the cause of oxidized arc magmas. Here, observations of …

Role of saline fluids in deep‐crustal and upper‐mantle metasomatism: insights from experimental studies

RC Newton, CE Manning - Geofluids, 2010 - Wiley Online Library
Geofluids (2010) 10, 58–72 Abstract Chloride‐rich brines are increasingly recognized as
playing an important role in high pressure and temperature metamorphic and magmatic …

Carbonate transfer during the onset of slab devolatilization: New insights from Fe and Zn stable isotopes

B Debret, P Bouilhol, ML Pons, H Williams - Journal of Petrology, 2018 - academic.oup.com
Long-term carbon cycling is a subject of recent controversy as new mass balance
calculations suggest that most carbon is transferred from the slab to the mantle wedge by …

The relationship between subduction zone redox budget and arc magma fertility

KA Evans, AG Tomkins - Earth and Planetary Science Letters, 2011 - Elsevier
A number of lines of evidence point to a causal link between oxidised slab-derived fluids,
oxidised sub-arc mantle, and the formation of economic concentrations of metals such as Cu …

COHS fluids released by oceanic serpentinite in subduction zones: Implications for arc-magma oxidation

WY Duan, XP Li, HP Schertl, AP Willner - Earth and Planetary Science …, 2022 - Elsevier
Subducted oceanic serpentinite carries H 2 O, ferric iron, carbon and sulfur into the
subduction zone, where they are stepwise released during dehydration. These COHS fluids …

[HTML][HTML] Iron-sulfur-carbon redox interactions in the continental subduction factory and their effect on volatile element storage in the mantle wedge

B Förster, S Aulbach, GE Bebout, G Bianchini… - Earth and Planetary …, 2024 - Elsevier
The ultramafic rocks of the Ulten Zone tectonic mélange experienced a well-documented
multi-stage metamorphic history, from residence in a hot mantle wedge to down-dragging …

Tracking Fe mobility and Fe speciation in subduction zone fluids at the slab-mantle interface in a subduction channel: A tale of whiteschist from the Western Alps

YX Chen, W Lu, Y He, HP Schertl, YF Zheng… - … et Cosmochimica Acta, 2019 - Elsevier
Fluids released by subducting slabs are important to the geochemical evolution of Earth's
crust-mantle system. However, it is still not well constrained for the mobility of redox sensitive …

[BOOK][B] The role of halogens in terrestrial and extraterrestrial geochemical processes: surface, crust, and mantle

DE Harlov, L Aranovich - 2018 - Springer
Terrestrial worlds on which H 2 O-bearing fluids are stable tend to show a higher degree of
chemical differentiation than similar worlds on which such fluids are not present or stable …