Abstract
Barite pseudomorphs after lenticular gypsum in a buried soil from central Australia are composed of loosely arranged platy crystals. These features were most probably formed by direct alteration with barium-rich solutions. The possible sources of the barium-rich solutions are briefly discussed.
| Original language | English |
|---|---|
| Pages (from-to) | 393-396 |
| Number of pages | 4 |
| Journal | Australian Journal of Soil Research |
| Volume | 31 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - 1993 |
| Externally published | Yes |