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In this paper, we find the internal stratification for terrestrial planetswith given mass-radius pairs, and use the core size and density to estimatetheir maximum dipolar magnetic moment. We also comment on the temporalevolution, although more information (e.g., core composition, mantle rheologyand history) is crucial in determining the state of the dynamo with planetaryage.

Predicted dynamos for terrestrial extra-solar planets and their influence in habitability