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Idealized IAB complex parent bodies with the preferred formation mechanisms for the MG and each of the subgroups, combining evidence from Mo and W isotope data (this study) with HSE data and observed silicate distributions among MG irons (Worsham et al., 2016a). Winonaites likely formed on the MG-sLL parent body (McCoy et al., 1993; Benedix et al., 2000). Relative parent body sizes are arbitrary.
