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Location: 83 km S from Kalgoorlie, Western Australia, Australia
Level 1 / 8 Richardson StreetPO Box 1810West PerthWestern Australia, Australia6005
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On July 25, 2023, Mincor Resources NL was removed from the Official List under Listing Rule 17.14, following the compulsory acquisition of its remaining securities by Wyloo Consolidated Investments Pty Ltd.
Wyloo Consolidated is wholly owned within the Wyloo Group, which in turn is wholly owned within the Tattarang Group.
The Widgiemooltha mineralisation is controlled by north-northwest trending structures and mainly hosted within basaltic rocks. Alteration assemblages consist of biotite-albite-carbonate and contain finely disseminated sulphides, mostly pyrite. The veining is dominantly quartz-carbonate with minor pyrite. Small aplite dykes, 1 m to 10 m thick, occur at Bass and Hronsky, and minor cherty-pyritic sediments and pegmatitic dykes at Flinders.Two ore morphologies can be identified at North Widgiemooltha, namely the steeply-dipping tabular lodes such as Bass and Hronsky, and the stacked shallow-dipping reef complexes hosting Flinders, Darlek and to a lesser extent West Oliver.There is only thin transported overburden in local areas (<3 m). The degree of weathering in the area varies with saprolite (100% weathered sulphides) from 0 to 15 m below the surface, while saprock (a mixture of weathered and unweathered sulphides) occurs down to 50 m depth.
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