Surface boulder banding indicates Martian debris-covered glaciers formed over multiple glaciations

Glacial landforms, including lobate debris aprons, are a global water ice reservoir on Mars preserving ice from past periods when high orbital obliquity permitted nonpolar ice accumulation. Numerous studies have noted morphological similarities between lobate debris aprons and terrestrial debris-cov...

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Veröffentlicht in:Proc Natl Acad Sci U S A
Hauptverfasser: Levy, Joseph S., Fassett, Caleb I., Holt, John W., Parsons, Reid, Cipolli, Will, Goudge, Timothy A., Tebolt, Michelle, Kuentz, Lily, Johnson, Jessica, Ishraque, Fairuz, Cvijanovich, Bronson, Armstrong, Ian
Format: Artigo
Sprache:Inglês
Veröffentlicht: National Academy of Sciences 2021
Schlagworte:
Physical Sciences
Online Zugang:https://ncbi.nlm.nih.gov/pmc/articles/PMC7848752/
https://ncbi.nlm.nih.gov/pubmed/33468681
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2015971118
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