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Fig. 13


Evolution of a Mercury-like planet in its disk (acore = 46 AU, Σ0 = 213.86 g cm-2, γ = 0.9). The migration of the planet through its life happened between 0.22 and 0.25 AU, where atomic Fe condensed in higher quantities than silicates (~65 wt % against ~30 wt %). Model “without”.

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