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By assuming that the cores of the planets contain both S and Si as light elements (Malavergne et al. 2007; Malavergne et al. 2010), the models of the thermal history of these planets suggest that, during their formation, the temperature in their centers approached or exceeded the liquidus temperature of the Fe Si S system after the magma ocean stage.
(1) Prolonged magma ocean stage.
This implies that circularization occurs during the magma ocean stage.
We find that tidal heating of a planetary mantle can influence surface habitability in several important ways: (1) Prolonged magma ocean stage.
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