Abstract
The mineral assemblage and paragenesis from Dale Head is interpreted in terms of phase equilibria and sulphidation data to estimate some of the conditions of formation of the sulfide ores.
Original language | English |
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Pages (from-to) | b25-b30 |
Number of pages | 6 |
Journal | Transactions of the Institution of Mining and Metallurgy, Section B: Applied Earth Science |
Volume | 89 |
Publication status | Published - 1980 |
Keywords
- Copper deposits