Kavli Affiliate: Paul D. Asimow | Summary:Iron disproportionation reactions in mantle silicates can produce metallic iron that drives Earth’s deep mantle toward metal saturation under reduced conditions. Subducting slabs transport hydrated silicates to these depths, where interactions with metallic iron can reduce structurally bound hydrogen in silicates to reduced hydrogen-bearing phases, such as molecular hydrogen […]
Continue.. Metal Saturation and the Redistribution of Hydrogen in Earth’s Mantle