GMRAP ID | 568 |
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Alternate names | Goodrich, Crown, Cyclops, Lady Lizzie, Sovereign, Sterling |
Tract name | Yeoval (009pCu8003) |
Site status | deposit |
Country | Australia |
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State or province | New South Wales |
Geographic location | 148.6432, -32.7283 |
Geologic map unit | 148.6432, -32.7283 |
Nearby data |
Deposit type | Porphyry copper |
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Age (Ma) | 411Ma |
Age determination method | Rb-Sr |
Age range | 411 ±2 Ma |
Age reference | Ambler and Facer (1975) |
Minerals | albite, azurite/malachite, biotite, bornite, carbonates, chalcopyrite, chlorite, copper, digenite, epidote, galena, gold, K-feldspar, magnetite, molybdenite, prehnite, pyrite, scheelite, sericite, silver, sphene |
Associated rocks | andesitic volcanics, diorite, gabbro, pyroxenite, dacite, dacite porphyry, granodiorite porphyry, quartz monzonite, greenstone- to amphibolite-facies meta-andesite, andesitic tuff and breccia, rhyolite, diorite, gabbro, limestone, shale |
Tectonic setting | continental margin |
Stratigraphic age | Early Devonian |
Development status | Prospect |
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Major commodities | Cu |
Minor commodities | Mo, Au, Ag |
Tonnage (Mt) | 13Mt |
Cu grade (%) | 0.38% |
Mo grade (%) | 0.012% |
Au grade (g/t) | 0.14g/t |
Ag grade (g/t) | 2.2g/t |
Contained copper | 49,000t |
Gold-Moly ratio | 12 |
Comments | Location, tonnage and grade of inferred resources from Geoscience Australia (2010); Ewers and others (2002) previously reported 20 Mt at 0.2% Cu, containing 40,000 t Cu + 300 t Cu produced. Veins, stockworks, disseminations; according to Ambler and Facer (1975), 27,000 t ore with 3% Cu and 15 g/t Au containing 800 t Cu and 0.4 t Au were mined; however, Jaireth and Miezitis (2004) reported production of only 300 t Cu and 0.159 t Au. |
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Study area name | Australia |
References | Gulson (1972); Gulson and Bofinger (1972); Ambler and Facer (1975); Bowman and others (1983); Paterson and others (1983); Ewers and others (2002); Wyborn and others (1987); Singer and others (2008); Augur Resources Ltd. (2009); Geoscience Australia (2010); Jaireth and Miezitis (2004) |
Site reference | Bookstrom and others (2014) |