Stringer-style FWZ mineralisation from the 735 Level in the Ming Mine (photograph taken in September 2024). The mineralisation consists of individual mm to cm scale chalcopyrite-pyrite veins hosted within highly chloritised rhyolite. This mineralisation is amenable to large-scale mining and often bulks out to grades exceeding 2% copper.
Stringer-style FWZ mineralisation from the 735 Level in the Ming Mine (photograph taken in September 2024). The mineralisation consists of individual mm to cm scale chalcopyrite-pyrite veins hosted within highly chloritised rhyolite. This mineralisation is amenable to large-scale mining and often bulks out to grades exceeding 2% copper.