
Image Credit: Malcolm Southwood

Image Credit: Malcolm Southwood

Image Credit: Malcolm Southwood



Title
dolomite after calcite (?)
Principal Mineral
Size
Cabinet; 95mm
Collection
Geoscience Australia R38858
Provenance
Smith, A.G.
Entry Type
Pseudomorph TSNB444
Description
An epimorphous "shell" of peach-coloured dolomite after calcite (?). The precursor mineral (probably calcite) has been completely disolved away leaving a ropey texture on the convex surface of the dolomite (Exhibit 1) and a pattern of angular molds on the concave surface (Exhibit 2). A side-by-side comparison of the two surfaces is presented in Exhibit 3. While not reliably diagnostic, these patterns are consistent with a trigonal carbonate, probably calcite, as the precursor mineral. The colour of the dolomite surfaces is likely due to the partial oxidation of iron in the dolomite lattice. There are no other minerals associated with the dolomite.
The specimen was formerly in the A. Glen Smith Collection which was donated to the Australian National Museum in the mid-1970s and is now housed at Geoscience Australia.
Associated Minerals
(not assigned)