Abstract
A micromorphological examination of some calcite pseudomorphs after lenticular gypsum in a deeply buried layer of an arid soil indicated that these features were formed by direct alteration. The likely changes in pedogenic environment that led to their formation are briefly discussed.
| Original language | English |
|---|---|
| Pages (from-to) | 483-485 |
| Number of pages | 3 |
| Journal | Australian Journal of Soil Research |
| Volume | 28 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - 1990 |
| Externally published | Yes |
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