Carbon dioxide in the martian seasonal polar caps can metamorphose into an annealed polycrystalline layer, provided freshly condensed grains are smaller than \(10 \mu \mathrm{m}\). Densification is not expected for coarse-grained (grain size larger than \(10 \mu \mathrm{m}\) ) \(\mathrm{CO}_{2}\) sn
The influence of the Martian polar caps on the diurnal tide
โ Scribed by Robert M. Haberle
- Publisher
- Elsevier Science
- Year
- 1979
- Tongue
- English
- Weight
- 829 KB
- Volume
- 39
- Category
- Article
- ISSN
- 0019-1035
No coin nor oath required. For personal study only.
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