Compositions of subsurface ices at the Mars Phoenix landing site
Author:
Affiliation:
1. Department of Earth and Planetary Sciences; Washington University in St. Louis; St. Louis; Missouri; USA
2. DEPARTMENT XXX; University of Colorado at Boulder; Boulder; Colorado; USA
3. NASA Johnson Space Center; Houston; Texas; USA
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/gl1024/2010GL045372/2010GL045372.pdf
Reference22 articles.
1. JSC Mars-1 - Martian regolith stimulant;Allen;Lunar Planet. Sci.,1997
2. Results from the Mars Phoenix Lander Robotic Arm experiment;Arvidson;J. Geophys. Res.,2009
3. D/H on Mars: Effects of floods, volcanism, impacts, and polar processes;Carr;Icarus,1990
4. A new model for Mars atmospheric dust based upon analysis of ultraviolet through infrared observations from Mariner 9, Viking, and Phobos;Clancy;J. Geophys. Res.,1995
5. Seasonal H2O and CO2 ice cycle at the Mars Phoenix landing site: 1. Prelanding CRISM and HiRISE observations;Cull;J. Geophys. Res.,2010
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