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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...

詳細記述

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書誌詳細
出版年:Geology
主要な著者: Chojnacki, Matthew, Banks, Maria E., Fenton, Lori K., Urso, Anna C.
フォーマット: Artigo
言語:Inglês
出版事項: 2019
主題:
オンライン・アクセス: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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