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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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| Publicado no: | Proc Natl Acad Sci U S A |
|---|---|
| Main Authors: | , , , , , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2021
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| Assuntos: | |
| Acesso em linha: | 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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