Landscape evolution in Martian mid-latitude regions: insights from analogous periglacial landforms in Svalbard
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چکیده
منابع مشابه
Origin of martian northern hemisphere mid-latitude lobate debris aprons
Lobate debris aprons in the martian midto high-latitudes (northern and southern hemispheres) have been interpreted as ice-related features that indicate periglacial climate conditions as recently as late Amazonian. Using MOLA topographic profiles perpendicular to apron flow fronts, we surveyed 36 debris aprons in the northern hemisphere found in the regions of Mareotis, Protonilus, and Deuteron...
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ژورنال
عنوان ژورنال: Geological Society, London, Special Publications
سال: 2011
ISSN: 0305-8719,2041-4927
DOI: 10.1144/sp356.7