Exploring Athabasca Subsurface Geoelectrical Properties Using MARSIS Radar Data: Hypothesis on Volcanic or Fluvial Origin of the Local Morphology

Details Exploring Athabasca Subsurface Geoelectrical Properties Using MARSIS Radar Data: Hypothesis on Volcanic or Fluvial Origin of the Local Morphology Exploring Athabasca Subsurface Geoelectrical Properties Using MARSIS Radar Data: Hypothesis on Volcanic or Fluvial Origin of the Local Morphology

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1819b&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Physics

Scientific paper

In this investigation, we explore the dielectric properties of the
martian subsurface in the equatorial area of Athabasca Vallis in order
to investigate whether they are consistent with the potential presence
of ground ice in this area.

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