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Location: 22 km SW from Orange, New South Wales, Australia
1460 Cadia Rd, CadiaOrangeNew South Wales, Australia2800
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The Ridgeway deposits are considered to be examples of alkalic porphyry gold copper-style mineralization.The deposit is a subvertical body of quartz-sulfide vein stockwork mineralization with an elliptical, pipe-like geometry, elongated along a northwest-striking axis. Stockwork dimensions are approximately 400 m east-west, 250 m north-south and the deposit extends to a depth in excess of 1,000 m.The top of the Ridgeway deposit is about 500 m below the surface and has approximate dimensions of 450 m east-west, 250 m north-south and extends about 1,000 m below the surface.Mineralization at Ridgeway and Ridgeway Deeps occurs in dense quartz vein stockworks and sheeted arrays localized in and around the small <50-100 m diameter) composite diorite to quartz-monzonite intrusive complex. The most strongly developed quartz stockwork veining and alteration, and the highest copper and gold grades, occur immediately adjacent to the monzonite.The frequency of the veins and intensity of alteration decreases away from the intrusive complex margin (Wilson et at., 2003). Ore minerals include bornite and chalcopyrite with lesser covellite and gold and occur in veins and as disseminations (Wilson et al., 2003).Sulfide minerals are zoned from a bomite to chalcopyrite (plus gold) core, outwards and upwards through a chalcopyrite-rich to an outer pyrite-rich domain.
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