Heat transport in the high-pressure ice mantle of large icy moons
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文摘
3D convection simulations tailored to specific structure of high-pressure ice mantle of large icy moons. Melting is introduced, melt extraction is assumed instantaneous. HP mantle found globally cold but small areas always at/close to the melting point in hot upwellings. Heat flux from rock core accomodated by melting at rock core interface and melt extraction throughout the HP ice mantle.

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