At the Sly Fox deposit gold mineralisation occurs in quartz veined and silica, pyrite, biotite altered schists
Regionally, the Dalgaranga project lies in the Archean aged Dalgaranga Greenstone Belt in the Murchison Province of Western Australia. At the Gilbey’s deposit, most gold mineralisation is associated with shears situated within biotite-sericite-carbonate pyrite altered schists with quartz-carbonate veining within a porphyry-shalemafic (dolerite, **bro, basalt) rock package (Gilbey’s Main Porphyry Zone). The Gilbey’s Main Porphyry Zone trends north – south and dips moderately-to-steeply to the west on local grid while Sly Fox deposit trends east – west and dips steeply to the north. These two trends define the orientation of the limbs of an anticlinal structure, with a highly disrupted area being evident in the hinge zone. •
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