Trace element partitioning on the Tinaquillo Lherzolite solidus at 1.5 GPa
The partition coefficient ( D ) for any trace element in the mantle is a function of pressure, temperature and phase composition, the latter of which is controlled by the relative fertility of the peridotite. Models of mantle melting therefore require accurate determination of partition coefficients...
| Hoofdauteurs: | , , |
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| Formaat: | Conference item |
| Gepubliceerd in: |
2003
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