Abstract
The oxide zones of a number of small historic mines and a large recent open-cut at Mineral Hill in central New South Wales have produced fine specimens of azurite, malachite, cerussite, cuprite and silver halides. Recent studies have revealed that volcanic-hosted mineralisation produced relatively simple secondary mineral assemblage of mainly azurite and malachite whereas sediment-hosted mineralisation yielded a far more complex secondary assemblage of oxide, carbonate, phosphate and sulfate minerals.
| Original language | English |
|---|---|
| Number of pages | 16 |
| Journal | Australian Journal of Mineralogy |
| Publication status | Published - 2005 |
Keywords
- New South Wales
- mineralogy
- azurite
- cerussite
- cuprite
- Condobolin
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