Isotopic evidence for iron mobility during subduction
(2016)
Journal Article
Debret, B., Millet, M., Pons, M., Bouilhol, P., Inglis, E., & Williams, H. (2016). Isotopic evidence for iron mobility during subduction. Geology, 44(3), 215-218. https://doi.org/10.1130/g37565.1
Subduction zones are one of the most important sites of chemical interchange between the Earth's surface and interior. One means of explaining the high Fe3+/ΣFe ratios and oxidized nature of primary arc magmas is the transfer of sulfate (SOX), carbon... Read More about Isotopic evidence for iron mobility during subduction.