Study reveals heterogeneous mantle source compositions for boninite from Bonin and Troodos
The δ56Fe isotope variation among different boninite sampling suites. Credit: IOCAS
Subduction-zone magmas are characterized by high fluid contents and Fe3+/ΣFe ratios, which are closely associated with slab-derived fluids during subduction. However, instead of a heavier iron isotope composition preferred under an oxidized state, arc magmas have lighter iron isotope compositions than seafloor basalts, including mid-ocean ridge…