I like this in the report "Gold mineralisation at Dixon occurs along the lithological contact of magnetite-rich dolerite and a non-magnetic dolerite, being identical to the mineralisation control observed at Gold Field’s Centenary Gold Mine6. (Prior to production in 1998, the Centenary gold resource was 8.4 million tonnes @ 7.7 g/t for 2.1 million ounces)7."
Ann: Quarterly Activities Report, page-2
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