Halogens and noble gases in modern and ancient oceanic lithosphere: Implications for subduction budgets and evolution of Earth's surface reservoirs
Noble gases and halogens are key tracers of volatile transport on Earth that can be incorporated into alteration minerals in the oceanic lithosphere and subducted to some degree back into Earth's mantle. The minerals and sites hosting these volatiles and the extent they are present in average oceanic lithosphere are subject to high uncertainties. Combined noble gases and halogen measurements were undertaken on samples of modern and ancient oceanic lithosphere, to study the incorporation and...[Show more]
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