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Location: 210 SE from Geraldton, Western Australia, Australia
Level 2, London House 216 St Georges TerracePerthWestern Australia, Australia6000
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Mt Karara magnetite mineralisation is confined to a magnetite banded iron formation (BIF) lithological unit that occurs within a tightly folded and structurally disrupted northeast trending syncline. The Mt Karara syncline is characterised by a thick western limb dipping steeply to the east and a thinner and more structurally complex eastern limb that dips less steeply to the west, and it is the thick western limb that hosts most of the interpreted mineralisation. Where drilling has penetrated the base of the BIF, the syncline structure is interpreted to plunge steeply to the north. The drilling coverage has allowed the Mt Karara deposit to be modelled to a strike length of approximately 3km and the main mineralised zone has a width of approximately 500m. The BIF has been interpreted to extend vertically to depths of >700m below the surface.
