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Boundary condition controls on the high-sand-flux regions of Mars

Wind has been an enduring geologic agent throughout the history of Mars, but it is often unclear where and why sediment is mobile in the current epoch. We investigated whether eolian bed-form (dune and ripple) transport rates are depressed or enhanced in some areas by local or regional boundary cond...

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Detalhes bibliográficos
Publicado no:Geology
Main Authors: Chojnacki, Matthew, Banks, Maria E., Fenton, Lori K., Urso, Anna C.
Formato: Artigo
Idioma:Inglês
Publicado em: 2019
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC7241575/
https://ncbi.nlm.nih.gov/pubmed/32440031
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1130/g45793.1
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