The Gaetani Lab

Experimental Petrology and Geochemistry
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    • Diffusive Re-equilibration of Olivine-Hosted Melt Inclusions
    • Aragonite/Seawater Partitioning of U/Ca
    • Upper Mantle Oxygen Fugacity
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High temperature

Low Temperature

Olivine-Hosted Melt Inclusions

Volatiles—such as water and carbon dioxide—play a central role in the generation and evolution of magmas deep within the Earth…. MORE

Aragonite/Seawater Partitioning of U/Ca

The aragonite skeleton of scleractinian corals contain coherent seasonal and interannual variability in U/Ca… MORE

Upper Mantle Oxygen Fugacity

The fugacity of oxygen in the oceanic upper mantle is a measure of the amount of oxygen available to react with elements that can exist in multiple valence states… MORE

Publications

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