Heat Flow from an Europa's Convective Ice Layer Tidally Heated

Details Heat Flow from an Europa's Convective Ice Layer Tidally Heated Heat Flow from an Europa's Convective Ice Layer Tidally Heated

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1035r&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1035

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Scientific paper

Convection in the ice shell is only compatible with high heat flows,
implies by Europa thin brittle lithosphere, if dominant tidal heating is
in the convective interior nearly isotherm, and if the ice viscosity is
dominated by superplastic flow.

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