Evidence for a Weakly Stratified Europan Ocean Sustained by Seafloor Heat Flux

Details Evidence for a Weakly Stratified Europan Ocean Sustained by Seafloor Heat Flux Evidence for a Weakly Stratified Europan Ocean Sustained by Seafloor Heat Flux

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1347t&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1347

Physics

Scientific paper

Chaos-type features on the surface of Europa are interpreted as
melt-through structures formed by rotationally confined oceanic plumes
that rise to the base of the ice shell from magmatically heated regions
of the seafloor.

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