Fuse Minerals is an exploration company focused on discovering mineral resources to support our future economy

Our strategy is what sets us apart from many exploration companies. It is a strategy designed to deliver short, medium, and long-term growth.

To meet the rapidly increasing demand for resources essential in the clean energy transition, established miners are starting to consider where they will be mining in ten, twenty, or thirty years from now. Fuse Minerals has developed a strategy, supported by the right projects and the right team, aimed at supplying tier 1 mining companies with the deposit discoveries they need to build the mines of the future.

The Fuse Minerals team is led by a group of experienced geologists and supported by members who bring extensive governance and corporate experience. Fuse Minerals has three prospective projects in copper, gold, silver, lead, and zinc. These projects are located in geological settings that can support the company's strategy

Fortuitously located in Western Australia between the Nifty, Woodie Woodie, Telfer, Havieron, and Winu. This is an area well recognised and tenure is secure.
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Situated on the complex boundary of two major tectonic units of Western Australia – the Proterozoic Gascoyne Province and the Palaeozoic Carnarvon Basin
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Featuring three Copper/Gold Projects located  in the Isaac region of Central Queensland. Mineralisation associated with copper & gold bearing cretaceous granodioritic intrusions (with historical copper mining) within the Bowen Basin sediments.
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First cab off the rank, the Mt Sydney Project

Surrounded by existing mines and development projects, systematic work has proven discovery potential.

History dominated by early-stage gold focused exploration or piecemeal work programmes before the 2017 VTEMmax survey. Multi-element rock chip samples generated positive base metal assays, yet there had been just 1,106m of drilling across the entire project.

Woodie Woodie Manganese Mine to the west and Nifty Copper Mine to the east. The project is located on the eastern margin of the Pilbara Craton, a location with mantle tapping structures and a setting suited to hosting various deposit styles.

VTEM survey, rock chipping and drilling intersecting volcanic hosted Cu/Zn sulphides suggests the 2.7 Ga Hardey Formation could host a VHMS camp.  With potential for magmatic Cu-Ni indicated by 4.5 x 1.1km coincident magnetic and conductive response in mafic rocks, plus malachite gossans in gabbro.

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