Fig. 6
Local induction heating and resulting temperature variations compared to a simulation without induction heating after 1 Gyr of thermal evolution. We show an example for 1.8 M⊕, iron content of 20 wt% and parameter case 3 for a fast rotator. Here, we only show the silicate mantle from the core radius of 2922 km to the planet radius of 7840 km.
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