Exploration for Challenger - type primary gold deposits that may possibly have formed within buried Archaean basement rocks in the Commonwealth Hill area, which is the purpose of one of two joint venture agreements currently in force between...
Exploration for Challenger - type primary gold deposits that may possibly have formed within buried Archaean basement rocks in the Commonwealth Hill area, which is the purpose of one of two joint venture agreements currently in force between Minotaur Gold and farminee Gawler Gold and Mineral Exploration, has consisted mostly of surface calcrete sampling and follow-up RAB/aircore and RC drilling of gold anomalies. In May 1997, the joint venture partners initially flew 12,944 line km of 100 m/200 m spaced regional aeromagnetic profiles across their contiguous exploration tenement package at Commonwealth Hill, generating structural targets which were then investigated with intensive geochemical analyses of 6569 auger-dug calcrete samples collected at prospect grid spacings ranging from 200m down to 50 m. More than 36 prospective anomalies were identified from this work, and 13 were subsequently drilled in a programme which is still continuing presently. So far, 956 RAB/aircore holes totalling 36,588 m, and 126 deeper angled RC holes totalling 14,985 m, have been completed by the joint venturers. Encouraging gold mineralisation has been encountered in both saprock and bedrock intervals in many of the drilled prospects, with the best early results being 12 m @ 1.0 g/t Au at Comet, 8 m @ 0.2 g/t Au at Neverfail, and 3 m @ 0.6 g/t Au at Birthday. The mineralisation is hosted by Archaean felsic and mafic granulites and occurs beneath a saprolite layer often up to 60 m thick. In addition to the gold grades, significantly anomalous base metals have been identified at Eaglehawk, Satellite, Neverfail, Isolation, St Andrews and Allanwater prospects, and an occurrence of high grade iron (28 m @ 53.4% Fe) was also found at St Andrews in association with gabbroic pyroxenite and microdolerite.
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