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Location: 20 km SE from Marble Bar, Western Australia, Australia
Corunna Downs RoadMarble BarWestern Australia, AustraliaWA 6760
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Mining scale, mining and mill throughput capaciites.Full profiles of select mines and projects.
Shaft depth, mining scale, backfill type and mill throughput data.Full profiles of select mines and projects.
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On 9 Oct 2024 - FTI Consulting were appointed as Deed Administrators of Calidus.
Deed of Company Arrangement (DOCA) proponent: West Coast Gold Pty Ltd.
On 8 Jan 2025 the Deed Administrators transferred all the Calidus shares to the DOCA Proponent’s nominee, Ample Resources Pty Ltd.
On 10 Jan 2025, the Deed Administrators confirmed to the DOCA Proponent that the Calidus DOCA, along with two DOCAS relating to its direct subsidiaries, Keras (Pilbara) Gold Pty Ltd and Calidus Blue Spec Pty Ltd, were wholly effectuated in accordance with their terms.
On 10 Jan 2025, the DOCA was effectuated: receivers and deed administrators retired, the company exited external administration, control passed to a new board, and Creditors’ Trusts were established with Hayden White and Daniel Woodhouse as Trustees.
Calidus delisted from ASX Jan 16, 2025.
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The Warrawoona Project leases lie within the Warrawoona Group, one of the oldest greenstone belts within the Pilbara Craton. Composed largely of high-Mg basaltic lavas with lesser tholeiite, andesite, sodic dacite, potassic rhyolite, chert and banded iron formation (BIF), all metamorphosed to greenschist facies, the Warrawoona Group is sandwiched between the Mount Edgar batholith to the north and the Corunna Downs batholith to the south. Gold occurs in quartz veins and stringers in the Klondyke, Copenhagen and Fieldings Gully Shears and mineralisation is associated with quartz-carbonate-sericite-pyrite alteration. Quartz veins and stringers are generally approximately parallel to the predominant shear direction. The bulk of the gold mineralisation is hosted in strongly sericitised and sheared mafic units with thin chert bands marking probable stratigraphic breaks. Over some abandoned workings gold mineralisation is associated with copper as indicated by the presence of malachite and other copper carbonates.The gold mineralisation identified to date at the Klondyke, Fieldings Gully and St George prospects consists of a number of interpreted mineralised lodes striking approximately 1350 and dipping steeply (80°-85°) to the north, Copenhagen has a similar strike but dips less steeply (at 70°) to the north. DimensionsAt Klondyke (KL), mineralisation has a sub-vertical dip as and ranges from 2m to 20m thick. The resource extends over approximately 5.1 km of strike and extends to a vertical depth of over 500 metres. The St George Trend mineralisation has a sub-vertical dip and ranges from approximately 1 m to 10 m thick with an approximate strike of 1.6 km extending to a vertical depth of approximately 200 m. The Resource is currently considered open along strike and down dip. Copenhagen Mineral Resources have a strike length of approximately 250 m with a steep southeasterly plunge and a steep northerly dip. Mineralised lodes range from 2m to 10m thick and extend to a vertical depth of 200m. Fieldings Gully mineralisation has a sub-vertical dip and ranges from 2m to 10m thick. The resource extends over approximately 440m of strike and extends to a vertical depth of 140m.
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