Ceres’ partial differentiation: undifferentiated crust mixing with a water-rich mantle

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Fig. 9

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Present temperature profiles for the cases shown in Figs. 5–7 in the same order as in Fig. 8. Dotted horizontal lines label the extension of the pure H₂ O layer, dashed vertical lines correspond to the melting point of ammonia dihydrate of 176 K and to that of pure H₂O ice of 273 K.

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