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A predictive model for rare earth element partitioning between clinopyroxene and anhydrous silicate melt

Abstract:

We present a quantitative model to describe the partitioning of rare earth elements (REE) and Y between clinopyroxene and anhydrous silicate melt as a function of pressure (P), temperature (T) and bulk composition (X). The model is based on the Brice (1975) equation, which relates the partition coefficient of element i (Di) to that element of o (Do) where the latter has the same ionic radius ro as the crystallographic site of interest, in this case the clinopyroxene M2 site: [see original art...

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Publication status:
Published

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Publisher copy:
10.1007/s004100050330

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Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Role:
Author
Journal:
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
Volume:
129
Issue:
2-3
Pages:
166-181
Publication date:
1997-10-05
DOI:
EISSN:
1432-0967
ISSN:
0010-7999
URN:
uuid:699d5c46-ca5a-4b7e-94f9-3bc4bf0b61d9
Source identifiers:
163813
Local pid:
pubs:163813
Language:
English

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