Soare, R.J.; Conway, S.; Pearce, G.D. and Costard, F.
PDF (Version of Record)
- Requires a PDF viewer such as GSview, Xpdf or Adobe Acrobat Reader
Download (249Kb) | Preview
|Google Scholar:||Look up in Google Scholar|
Landforms suggestive of periglacial processes are commonplace in mid-Utopia Planitia, Mars. They form syngenetically in ground-ice comprised of loess transported by katabatic wind from the NPLDs and enriched by ice through the thaw-freeze cycling of obliquity-driven precipitation.
|Item Type:||Conference Item|
|Copyright Holders:||2012 LPI|
|Academic Unit/Department:||Science > Physical Sciences
|Depositing User:||Susan Conway|
|Date Deposited:||06 Nov 2012 09:41|
|Last Modified:||26 Feb 2016 03:03|
|Share this page:|
Download history for this item
These details should be considered as only a guide to the number of downloads performed manually. Algorithmic methods have been applied in an attempt to remove automated downloads from the displayed statistics but no guarantee can be made as to the accuracy of the figures.