Abstract
We defend the position taken in our earlier note that under certain conditions the D/H ratio measured in the coma of a comet can be much higher that the D/H ratio in to cometary ice itself.
| Original language | English |
|---|---|
| Pages (from-to) | 221-222 |
| Number of pages | 2 |
| Journal | Icarus |
| Volume | 168 |
| Issue number | 1 |
| DOIs | |
| State | Published - Mar 2004 |
Keywords
- Comet, composition
- Comets, origin
- Ices
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