The micromorphology and elemental composition of celestobarite crystal
s in a duripan from central Australia are examined. These crystals are
flabellate (fan-shaped), have a Ba/Sr ratio of 11.1, and are up to 50
mu m in size. The location of the celestobarite crystals within silic
ified roots and in close association with calcite and clay coatings in
dicates that these celestobarite crystals are authigenic and were form
ed under aridic environments.