Cold-based glaciation of Pavonis Mons, Mars: evidence for moraine deposition during glacial advance

The three large volcanoes in the Tharsis region of Mars: Arsia, Pavonis, and Ascraeus Montes all have fan-shaped deposits (FSDs) on their northern or western flanks consisting of a combination of parallel ridges, knobby/hummocky terrain, and a smooth, viscous flow-like unit. The FSDs are hypothesize...

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Detalles Bibliográficos
Autores principales: Parsons, Reid A., Kanzaki, Tomohiro, Hemmi, Ryodo, Miyamoto, Hideaki
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2020
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7194259/
https://www.ncbi.nlm.nih.gov/pubmed/32382472
http://dx.doi.org/10.1186/s40645-020-0323-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7194259/
https://www.ncbi.nlm.nih.gov/pubmed/32382472
http://dx.doi.org/10.1186/s40645-020-0323-9

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