Experimental and computational study of trace element distribution between orthopyroxene and anhydrous silicate melts: substitution mechanisms and the effect of iron

M. van Kan - Parker; A. Liebscher; D. Frei; J. van Sijl; W. van Westrenen; J.D. Blundy; G. Franz

doi:10.1007/s00410-009-0435-0

Experimental and computational study of trace element distribution between orthopyroxene and anhydrous silicate melts: substitution mechanisms and the effect of iron

M. van Kan - Parker
, A. Liebscher
, D. Frei
, J. van Sijl
, W. van Westrenen
, J.D. Blundy
, G. Franz

Research output: Contribution to Journal › Article › Academic › peer-review

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Abstract

Although orthopyroxene (Opx) is present during a wide range of magmatic differentiation processes in the terrestrial and lunar mantle, its effect on melt trace element contents is not well quantified. We present results of a combined experimental and computational study of trace element partitioning between Opx and anhydrous silicate melts. Experiments were performed in air at atmospheric pressure and temperatures ranging from 1,326 to 1,420°C in the system CaO-MgO-Al

Original language	English
Pages (from-to)	459-473
Journal	Contributions to Mineralogy and Petrology
Volume	159
Issue number	4
DOIs	https://doi.org/10.1007/s00410-009-0435-0
Publication status	Published - 2010

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van Kan - Parker, M., Liebscher, A., Frei, D., van Sijl, J., van Westrenen, W., Blundy, J. D., & Franz, G. (2010). Experimental and computational study of trace element distribution between orthopyroxene and anhydrous silicate melts: substitution mechanisms and the effect of iron. Contributions to Mineralogy and Petrology, 159(4), 459-473. https://doi.org/10.1007/s00410-009-0435-0

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abstract = "Although orthopyroxene (Opx) is present during a wide range of magmatic differentiation processes in the terrestrial and lunar mantle, its effect on melt trace element contents is not well quantified. We present results of a combined experimental and computational study of trace element partitioning between Opx and anhydrous silicate melts. Experiments were performed in air at atmospheric pressure and temperatures ranging from 1,326 to 1,420°C in the system CaO-MgO-Al",

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van Kan - Parker, M, Liebscher, A, Frei, D, van Sijl, J, van Westrenen, W, Blundy, JD & Franz, G 2010, 'Experimental and computational study of trace element distribution between orthopyroxene and anhydrous silicate melts: substitution mechanisms and the effect of iron', Contributions to Mineralogy and Petrology, vol. 159, no. 4, pp. 459-473. https://doi.org/10.1007/s00410-009-0435-0

Experimental and computational study of trace element distribution between orthopyroxene and anhydrous silicate melts: substitution mechanisms and the effect of iron. / van Kan - Parker, M.; Liebscher, A.; Frei, D. et al.
In: Contributions to Mineralogy and Petrology, Vol. 159, No. 4, 2010, p. 459-473.

Research output: Contribution to Journal › Article › Academic › peer-review

TY - JOUR

T1 - Experimental and computational study of trace element distribution between orthopyroxene and anhydrous silicate melts: substitution mechanisms and the effect of iron

AU - van Kan - Parker, M.

AU - Liebscher, A.

AU - Frei, D.

AU - van Sijl, J.

AU - van Westrenen, W.

AU - Blundy, J.D.

AU - Franz, G.

PY - 2010

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AB - Although orthopyroxene (Opx) is present during a wide range of magmatic differentiation processes in the terrestrial and lunar mantle, its effect on melt trace element contents is not well quantified. We present results of a combined experimental and computational study of trace element partitioning between Opx and anhydrous silicate melts. Experiments were performed in air at atmospheric pressure and temperatures ranging from 1,326 to 1,420°C in the system CaO-MgO-Al

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DO - 10.1007/s00410-009-0435-0

M3 - Article

SN - 0010-7999

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JO - Contributions to Mineralogy and Petrology

JF - Contributions to Mineralogy and Petrology

IS - 4

ER -

Experimental and computational study of trace element distribution between orthopyroxene and anhydrous silicate melts: substitution mechanisms and the effect of iron

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