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Compaction-Driven Evolution of Pluto's Rocky Core: Implications for Water-Rock Interactions

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Leila Gabasova, Institut de Planétologie et Astrophysique de Grenoble, models the compaction of Pluto's rocky core after accretion and explore the potential for hydrothermal circulation within the porous layer, as well as examine its effect on core cooling and the persistence of a liquid internal ocean.

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