Abstract
Naturally occurring chromate minerals are confined to the oxidized zones of base metal orebodies and to extremely oxidizing desert environments. Under such conditions, chromium reaches its highest oxidation state (+6).
| Original language | English |
|---|---|
| Title of host publication | Encyclopedia of Geology |
| Place of Publication | The Netherlands |
| Publisher | Elsevier |
| Pages | 532-534 |
| Number of pages | 3 |
| ISBN (Print) | 0126363803 |
| DOIs | |
| Publication status | Published - 2005 |
Keywords
- chromate
- minerals
- oxidization
- chromium
- chromite