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- W1566881149 abstract "Experiments on C(graphite)+basaltic melt and C(graphite)+Mg2SiO4+melt, C(graphite)+Mg2SiO4+(CO‐CO2) vapor+melt at 15‐40 kbar, 1400‐1700 °C have shown that carbon may be soluble in forsterite and pyroxene in concentrations of 10‐100 ppm, and reactions with graphite lead to formation in the melt of 100‐1000 ppm CO2 concentrations. Carbon is an incompatible element in the melt+crystals system. The redox state of the mantle and interactions among primary carbon, melt and crystals are suggested to play an important role in the formation of carbon species in terrestrial basalts." @default.
- W1566881149 created "2016-06-24" @default.
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- W1566881149 date "1995-01-01" @default.
- W1566881149 modified "2023-09-25" @default.
- W1566881149 title "Formation of carbon species in terrestrial magmas" @default.
- W1566881149 doi "https://doi.org/10.1063/1.48734" @default.
- W1566881149 hasPublicationYear "1995" @default.
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