Abstract
The thermal evolution of Europa is described by a new path of geophysical development. Petrological considerations suggest that heat may have been transported within Europa by sub-solidus convection, and that a large fraction of Europa's water content is retained as hydrated silicates.
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Ransford, G., Finnerty, A. & Collerson, K. Europa's petrological thermal history. Nature 289, 21–24 (1981). https://doi.org/10.1038/289021a0
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DOI: https://doi.org/10.1038/289021a0
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