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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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| Vydáno v: | Geology |
|---|---|
| Hlavní autoři: | , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
2019
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| Témata: | |
| On-line přístup: | 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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