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...
| Autores principales: | , , |
|---|---|
| Formato: | Journal article |
| Lenguaje: | English |
| Publicado: |
2001
|