Mid-Latitude Dissected Mantle Terrain as Viewed from HiRISE

Details Mid-Latitude Dissected Mantle Terrain as Viewed from HiRISE Mid-Latitude Dissected Mantle Terrain as Viewed from HiRISE

Jul 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpico1353.3351s&link_type=abstract

Seventh International Conference on Mars, held July 9-13, 2007 in Pasadena, California, LPI Contribution No. 1353, p.3351

Physics

Scientific paper

Using HiRISE, we examine the morphology of the mid-latitude dissected
mantle terrain to test the plausibility of the hypothesis that this
global terrain results from desiccation of an ice-rich mantle deposited
at times of high obliquity.

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