Abstract
At temperatures above about 1100° C degassed molten kimberlites were found to attack diamond, producing both graphite and metallic iron on the diamond surface. Using ordinary kimberlites in experiments performed at 1 Kb in a closed system, diamonds developed etch features (at temperatures above about 1000° C), consistent with attack by wet CO2, but no graphite or iron was formed on the surfaces of the diamonds.
| Original language | English |
|---|---|
| Pages (from-to) | 237-244 |
| Number of pages | 8 |
| Journal | Contributions to Mineralogy and Petrology |
| Volume | 47 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - Dec 1974 |
| Externally published | Yes |
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