CORDIS Project
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The OZ project explores the interactions of fluids in subduction zones to understand Earth's redox processes. It aims to determine how these interactions affect the oxidation of the mantle and the generation of arc magmatism through experimental and modeling approaches.
In contrast to other known terrestrial planets, the Earth's interior is oxygen-breathing through the sink of oxidised tectonic plates at convergent margins since the late Archean to Paleoproterozoic.
Recent estimates suggest that the redox capacity of some key subducting chemical elements is not balanced on geological time scales by global magmatism and volcanism, thus implying a puzzling deep oxygenation of our planet.
Although current models presume that the redox state of subducting slabs is…
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