Fig. 4
Same as Fig. 3, but using a fragmentation velocity of uf = 10 m s−1. Starting from the outer boundary, for α = 10−3 the species that evaporate are CO2, H2O, Fe3O4, C, and FeS. For α = 5 × 10−4 the ice lines are of CO2, H2O, Fe3O4, C, and FeS and for α = 10−4 they are CO2 and H2O. The water ice line is shown as a dashed line.
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