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

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Fig. 8

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Evolution of the critical viscosity for the occurrence of Rayleigh-Taylor instabilities (red) and evolution of the viscosity at the base of the crust (blue) for the cases shown in Figs. 5–7. Top row: models from left to right and top to bottom in order of their appearance in Figs. 5–7.

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