The behavior of iron and zinc stable isotopes accompanying the subduction of mafic oceanic crust: A case study from Western Alpine ophiolites
(2017)
Journal Article
Inglis, E. C., Debret, B., Burton, K. W., Millet, M., Pons, M., Dale, C. W., …Williams, H. M. (2017). The behavior of iron and zinc stable isotopes accompanying the subduction of mafic oceanic crust: A case study from Western Alpine ophiolites. Geochemistry, Geophysics, Geosystems, 18(7), 2562-2579. https://doi.org/10.1002/2016gc006735
Arc lavas display elevated Fe3+/ΣFe ratios relative to MORB. One mechanism to explain this is the mobilization and transfer of oxidised or oxidising components from the subducting slab to the mantle wedge. Here we use iron and zinc isotopes, which ar... Read More about The behavior of iron and zinc stable isotopes accompanying the subduction of mafic oceanic crust: A case study from Western Alpine ophiolites.