CO2 solubility and speciation in rhyolitic sediment partial melts at 1.5–3.0GPa – Implications for carbon flux in subduction zones
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Reevaluating carbon fluxes in subduction zones, what goes down, mostly comes upCarbon contents in reduced basalts at graphite saturation: Implications for the degassing of Mars, Mercury, and the MoonCO2 content of andesitic melts at graphite-saturated upper mantle conditions with implications for redox state of oceanic basalt source regions and remobilization of reduced carbon from subducted eclogiteRise of Earth’s atmospheric oxygen controlled by efficient subduction of organic carbonCarbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryosEffect of melt composition on crustal carbonate assimilation: Implications for the transition from calcite consumption to skarnification and associated CO2degassingPartial 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 margins
P2860
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P2860
CO2 solubility and speciation in rhyolitic sediment partial melts at 1.5–3.0GPa – Implications for carbon flux in subduction zones
description
im Jahr 2014 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в січні 2014
@uk
name
CO2 solubility and speciation ...... arbon flux in subduction zones
@en
CO2 solubility and speciation ...... arbon flux in subduction zones
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type
label
CO2 solubility and speciation ...... arbon flux in subduction zones
@en
CO2 solubility and speciation ...... arbon flux in subduction zones
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prefLabel
CO2 solubility and speciation ...... arbon flux in subduction zones
@en
CO2 solubility and speciation ...... arbon flux in subduction zones
@nl
P1476
CO2 solubility and speciation ...... arbon flux in subduction zones
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P2093
Megan S. Duncan
P304
P356
10.1016/J.GCA.2013.09.026
P577
2014-01-01T00:00:00Z