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

Lunar and Planetary Lab

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

ASJC Scopus subject areas

Environmental Science(all)
Earth and Planetary Sciences(all)

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10.1111/j.1945-5100.1988.tb00898.x

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

Abstract

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