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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Detalles Bibliográficos
Autores principales: 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
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2021
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7848752/
https://www.ncbi.nlm.nih.gov/pubmed/33468681
http://dx.doi.org/10.1073/pnas.2015971118

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7848752/
https://www.ncbi.nlm.nih.gov/pubmed/33468681
http://dx.doi.org/10.1073/pnas.2015971118

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