The Fate of Sulfur During Fluid-Present Melting of Subducting Basaltic Crust at Variable Oxygen Fugacity
about
Redox processes in subducting oceanic crust recorded by sulfide-bearing high-pressure rocks and veins (SW Tianshan, China)Partial melting of fertile peridotite fluxed by hydrous rhyolitic melt at 2–3 GPa: implications for mantle wedge hybridization by sediment melt and generation of ultrapotassic magmas in convergent marginsEffect of variable CO2on eclogite-derived andesite and lherzolite reaction at 3 GPa-Implications for mantle source characteristics of alkalic ocean island basalts
P2860
The Fate of Sulfur During Fluid-Present Melting of Subducting Basaltic Crust at Variable Oxygen Fugacity
description
im Mai 2014 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в травні 2014
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name
The Fate of Sulfur During Flui ...... st at Variable Oxygen Fugacity
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The Fate of Sulfur During Flui ...... st at Variable Oxygen Fugacity
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type
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The Fate of Sulfur During Flui ...... st at Variable Oxygen Fugacity
@en
The Fate of Sulfur During Flui ...... st at Variable Oxygen Fugacity
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prefLabel
The Fate of Sulfur During Flui ...... st at Variable Oxygen Fugacity
@en
The Fate of Sulfur During Flui ...... st at Variable Oxygen Fugacity
@nl
P2860
P356
P1433
P1476
The Fate of Sulfur During Flui ...... st at Variable Oxygen Fugacity
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P2093
Sébastien Jégo
P2860
P304
P356
10.1093/PETROLOGY/EGU016
P577
2014-05-29T00:00:00Z