Periods of active permafrost layer formation during the geological history of Mars: Implications for circum-polar and mid-latitude surface processes
Authors:
- Mikhail A. KreslavskyMKMikhail A. Kreslavsky
- James W. HeadJHJames W. Head
- David R. MarchantDMDavid R. Marchant
- 1 February 2008
- journal article
- Published by Elsevier in Planetary and Space Science
- Vol. 56 (2) , 289-302
Abstract
No abstract availableThis publication has 58 references indexed in Scilit:
- Mars at very low obliquity: Atmospheric collapse and the fate of volatilesGeophysical Research Letters, 2005
- Ice‐driven creep on Martian debris slopesGeophysical Research Letters, 2003
- On the orbital forcing of Martian water and CO2 cycles: A general circulation model study with simplified volatile schemesJournal of Geophysical Research, 2003
- Redistribution of water in terrestrial soils at subfreezing temperatures: A review of processes and their potential relevance to MarsJournal of Geophysical Research, 2003
- Mars: Nature and evolution of young latitude‐dependent water‐ice‐rich mantleGeophysical Research Letters, 2002
- Kilometer‐scale roughness of Mars: Results from MOLA data analysisJournal of Geophysical Research, 2000
- Improved general circulation models of the Martian atmosphere from the surface to above 80 kmJournal of Geophysical Research, 1999
- Kilometer‐scale slopes on Mars and their correlation with geologic units: Initial results from Mars Orbiter Laser Altimeter (MOLA) dataJournal of Geophysical Research, 1999
- The distribution and behavior of Martian ground ice during past and present epochsJournal of Geophysical Research, 1995
- Chaotic obliquity and the nature of the Martian climateJournal of Geophysical Research, 1995