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-shale-mafic (dolerite, gabbro, basalt) rock package (Gilbey’s Main Porphyry Zone and Sly Fox). The Gilbey’s Main Porphyry Zone trends north – south and dips moderately-to-steeply to the west on local grid while Sly Fox 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.
At the Sly Fox deposit gold mineralisation occurs in quartz veined and silica, pyrite, biotite altered schists.
The Plymouth deposit lies between Gilbey’s and Sly Fox within the hinge zone of anticlinal structure – mineralisation at Plymouth is related to quartz veins and silica, pyrite, biotite altered schists.
At Hendricks and Vickers gold mineralisation occurs in quartz-pyrite veined and altered zones hosted in basalts.
The Never Never deposit at Gilbey’s North appears to be an intersection between a significant mineralised structure and the mine sequence – the lode plunges moderately to the west and is characterised by strong quartz – sericite – fucite alteration, with fine to very fine pyrite ........
