Discovery Projects - Grant ID: DP0450252

Funding Activity

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Funded Activity Summary

The geochemical role of iron in basaltic magmatism and planetary differentiation: an experimental study. The amount of Fe in primitive terrestrial basalts is surprisingly variable. The reasons for this are poorly understood, but could include melting of Fe-enriched refertilized mantle sources, increasing partitioning of FeO into the melt with depth of melting, or oxidation of some FeO to Fe2O3. An experimental investigation of the effects of Fe both as 2+ and 3+ on the partial melting of model mantle material should help resolve this problem, while also providing the fundamental thermodynamic data needed to calibrate a general model for upper mantle phase relations.

Funded Activity Details

Start Date: 01-01-2004

End Date: 31-12-2006

Funding Scheme: Discovery Projects

Funding Amount: $105,000.00

Funder: Australian Research Council