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...
Κύριοι συγγραφείς: | van Westrenen, W, Wood, B, Blundy, J |
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Μορφή: | Journal article |
Γλώσσα: | English |
Έκδοση: |
2001
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Παρόμοια τεκμήρια
Παρόμοια τεκμήρια
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Crystal-chemical controls on trace element partitioning between garnet and anhydrous silicate melt
ανά: van Westrenen, W, κ.ά.
Έκδοση: (1999) -
Atomistic simulation of trace element incorporation into garnets - comparison with experimental garnet-melt partitioning data
ανά: van Westrenen, W, κ.ά.
Έκδοση: (2000) -
Effect of Fe2+ on garnet-melt trace element partitioning: experiments in FCMAS and quantification of crystal-chemical controls in natural systems
ανά: van Westrenen, W, κ.ά.
Έκδοση: (2000) -
High field strength element/rare earth element fractionation during partial melting in the presence of garnet: Implications for identification of mantle heterogeneities
ανά: van Westrenen, W, κ.ά.
Έκδοση: (2001) -
Partitioning of trace elements between crystals and melts
ανά: Blundy, J, κ.ά.
Έκδοση: (2003)