Ice Melting Above a Convecting, Crystallizing Magmatic Sill on Mars

Details Ice Melting Above a Convecting, Crystallizing Magmatic Sill on Mars Ice Melting Above a Convecting, Crystallizing Magmatic Sill on Mars

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2275m&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2275

Physics

Scientific paper

We investigate the melting of an ice layer above a vigorously
convecting, crystallizing magmatic sill intruded in the martian crust.
We show that the melt layer is 3.5 times the sill thickness, assuming
crystals remain suspended in the melt.

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