Partioning of rare earth elements between hibonite and melt and implications for nebular condensation of the rare earth elements

M. J. Drake; W. V. Boynton

doi:10.1111/j.1945-5100.1988.tb00898.x

Partioning of rare earth elements between hibonite and melt and implications for nebular condensation of the rare earth elements

M. J. Drake
, W. V. Boynton

Research output: Contribution to journal › Article › peer-review

19 Scopus citations

Abstract

The partitioning of the rare earth elements between hibonite and silicate melt has been investigated at 1470°C in the system calcium tschermak's molecule-diopside. Results suggest that unless the principal phase(s) into which a trace element is dissolving and the activity-composition relationships for that trace element in that phase(s) are known, condensation temperatures based on assumed ideal solution behavior will generally be in error. -from Authors

Original language	English (US)
Pages (from-to)	75-80
Number of pages	6
Journal	Meteoritics
Volume	23
Issue number	1
DOIs	https://doi.org/10.1111/j.1945-5100.1988.tb00898.x
State	Published - 1988
Externally published	Yes

ASJC Scopus subject areas

General Environmental Science
General Earth and Planetary Sciences

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10.1111/j.1945-5100.1988.tb00898.x

Cite this

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abstract = "The partitioning of the rare earth elements between hibonite and silicate melt has been investigated at 1470°C in the system calcium tschermak's molecule-diopside. Results suggest that unless the principal phase(s) into which a trace element is dissolving and the activity-composition relationships for that trace element in that phase(s) are known, condensation temperatures based on assumed ideal solution behavior will generally be in error. -from Authors",

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year = "1988",

doi = "10.1111/j.1945-5100.1988.tb00898.x",

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Y1 - 1988

N2 - The partitioning of the rare earth elements between hibonite and silicate melt has been investigated at 1470°C in the system calcium tschermak's molecule-diopside. Results suggest that unless the principal phase(s) into which a trace element is dissolving and the activity-composition relationships for that trace element in that phase(s) are known, condensation temperatures based on assumed ideal solution behavior will generally be in error. -from Authors

AB - The partitioning of the rare earth elements between hibonite and silicate melt has been investigated at 1470°C in the system calcium tschermak's molecule-diopside. Results suggest that unless the principal phase(s) into which a trace element is dissolving and the activity-composition relationships for that trace element in that phase(s) are known, condensation temperatures based on assumed ideal solution behavior will generally be in error. -from Authors

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U2 - 10.1111/j.1945-5100.1988.tb00898.x

DO - 10.1111/j.1945-5100.1988.tb00898.x

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Partioning of rare earth elements between hibonite and melt and implications for nebular condensation of the rare earth elements

Abstract

ASJC Scopus subject areas

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