Regular ArticleCore Sizes and Internal Structure of Earth's and Jupiter's Satellites
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2022, Geochimica et Cosmochimica ActaPlanetary core radii: from Plato towards PLATO
2022, Advances in GeophysicsCitation Excerpt :Two different ranges for the core radius resulted, depending on the presence or absence of Sulfur in the core. In a subsequent study (Kuskov and Kronrod, 2001), with a slightly more complex set of building blocks, these radius ranges were modified and narrowed down. In both studies, Kuskov and Kronrod concluded with regard to the origin of the Moon that “The chemical composition of the Moon is different from that of the Earth's upper mantle and bears no genetic relationship to the terrestrial material as well as to any of the known chondrites.” (
Top-down freezing in a Fe–FeS core and Ganymede's present-day magnetic field
2018, IcarusCitation Excerpt :Ganymede’s magnetic field is mainly dipolar with an equatorial field strength of 719 nT (Kivelson et al., 2002). The existence of the magnetic field and the low mean moment of inertia (MOI) factor of 0.3105 (Anderson et al., 1996) strongly suggest a metallic core for Ganymede (Sohl et al., 2002; Kuskov and Kronrod, 2001). An active dynamo in this core is the most probable explanation for the observed strong field (Schubert et al., 1996).
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2016, Physics of the Earth and Planetary Interiors