Effect of oxygen fugacity on the H sub(2)O storage capacity of forsterite in the carbon-saturated systems

High pressure experiments have been performed in the systems Mg sub(2)SiO sub(4)-C-O-H and Mg sub(2)SiO sub(4)-K sub(2)CO sub(3)-C at 6.3 GPa and 1200 to 1600 C using a split-sphere multi-anvil apparatus. In the Mg sub(2)SiO sub(4)-C-O-H system the composition of fluid was modeled by adding differen...

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Veröffentlicht in:	Geochimica et cosmochimica acta 2010-08, Vol.74 (16), p.4793-4806
Hauptverfasser:	Sokol, Alexander G, Palyanov, Yury N, Kupriyanov, Igor N, Litasov, Konstantin D, Polovinka, Mariya P
Format:	Artikel
Sprache:	eng
Schlagworte:	Buffers Computational fluid dynamics Fluid flow Fluids Forsterite Melts Olivine Solidus
Online-Zugang:	Volltext
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