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 |
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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 |