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Parental arc magma compositions dominantly controlled by mantle-wedge thermal structure

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Parental arc magma compositions dominantly controlled by mantle-wedge thermal structure

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Fully-coupled 3D modelling of magmatic dike Propagation – finite pulse release from a point source

Mercury Isotope Fractionation during Dark Abiotic Reduction of Hg(II) by Dissolved, Surface-Bound, and Structural Fe(II)

Persistence of the isotopic signature of pentavalent uranium in magnetite

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