The effect of oxygen fugacity on the solubility of carbon-oxygen fluids in basaltic melt

The solubility of CO 2 CO fluids in a mid-ocean ridge basalt ( morb) has been measured at 1200°C, 500–1500 bar, and oxygen fugacities between NNO and NNO-4. High oxygen fugacities, and thus CO 2-rich fluids, were produced by using a starting material equilibrated at NNO, and Ag 2C 2O 4 as the fluid...

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Veröffentlicht in:	Earth and planetary science letters 1992-05, Vol.110 (1), p.213-225
Hauptverfasser:	Pawley, Alison R., Holloway, John R., McMillan, Paul F.
Format:	Artikel
Sprache:	eng
Schlagworte:	Crystalline rocks Earth sciences Earth, ocean, space Exact sciences and technology Experimental petrology
Online-Zugang:	Volltext
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