A predictive thermodynamic model of garnet-melt trace element partitioning
We have developed a predictive model for the partitioning of magnesium and a range of trivalent trace elements (rare earth elements, Y, In and Sc) between garnet and anhydrous silicate melt as a function of pressure, temperature and bulk composition. The model for the magnesium partition coefficient...
Prif Awduron: | van Westrenen, W, Wood, B, Blundy, J |
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Fformat: | Journal article |
Iaith: | English |
Cyhoeddwyd: |
2001
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Eitemau Tebyg
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Crystal-chemical controls on trace element partitioning between garnet and anhydrous silicate melt
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Atomistic simulation of trace element incorporation into garnets - comparison with experimental garnet-melt partitioning data
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Effect of Fe2+ on garnet-melt trace element partitioning: experiments in FCMAS and quantification of crystal-chemical controls in natural systems
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High field strength element/rare earth element fractionation during partial melting in the presence of garnet: Implications for identification of mantle heterogeneities
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Partitioning of trace elements between crystals and melts
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