The Response of Martian Ground Ice to Burial by a Volatile-Poor Mantle: Potential Implications for the Volatile Evolution of the Medusae Fossae Formation

Details The Response of Martian Ground Ice to Burial by a Volatile-Poor Mantle: Potential Implications for the Volatile Evolution of the Medusae Fossae Formation The Response of Martian Ground Ice to Burial by a Volatile-Poor Mantle: Potential Implications for the Volatile Evolution of the Medusae Fossae Formation

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2142c&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2142

Physics

Scientific paper

We consider the thermal and volatile response of an ice-rich martian
crust to burial by an initially dry porous mantle of sediment or
volcanic ash.

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