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 |
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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 |