High Grade Iron Rock Chip Results at Robinson Range – Bryah Basin

CuFe Ltd (ASX: CUF) (CuFe or the Company) is pleased to provide an update on its exploration activities within E52/1613, part of the Bryah Basin Project portfolio.

HIGHLIGHTS

• High grade iron enrichment identified on CuFe Bryah Basin Tenement E52/1613.
• Early-stage reconnaissance field work yields rock chip assays up to 60.63% Fe with low impurities.
• Corridor of surface supergene enrichment of Banded Iron Formation identified that has the potential to extend for 1.2km strike length.
• Full field mapping and rock chip program planned later this quarter.

Although this is not the highest priority within our portfolio (where the focus is on exploration targets for future facing minerals including copper at Tennant Creek, lithium at North Dam and niobium in the West Arunta), we will follow up with more mapping and sampling along strike to further test the potential and to identify drill targets. The project logistics are favourable and offer potential for the style of low Capex DSO project we have experience in developing and executing.”

Tenement Overview

The CuFe Bryah Basin Project includes a package of tenements under various joint ventures and farm-ins, with a primary focus on the potential for gold and copper mineralisation. During a strategic review of the tenure CuFe identified that tenement E52/1613 has the potential for iron ore hosted within the Banded Iron Formation of the Robinson Range. E52/1613 is 100% owned by CuFe’s subsidiary Jackson Minerals following the withdrawal of the tenement from the Auris Minerals Ltd JV in the March 24 quarter.

The tenement covers an area of 34km² and is located approximately 95km north of the township of Meekatharra and 630km east of the Port of Geraldton, in the Midwest / Murchison Region of Western Australia (Figure 1). The Great Northern Highway passes 10km to the south, and the Ashburton Downs- Meekatharra Road passes 15km to the west of the tenement. Several roads and pastoral station tracks extend from these major transport routes and provide excellent access to the project area.

Figure 1: E52/1613 Location – Bryah Basin.

Local Geology and Iron Mineralisation

The project area and more extensively the Robinson Range Formation lies within Bryah-Padbury Basin which is part of the Proterozoic Capricorn Orogenic Belt lying between the Pilbara and Yilgarn Archaean Cratons. The Robinson Range Formation occurs toward the upper part of the Palaeoproterozoic Padbury Group. It contains Banded Iron Formations (BIF) and hematitic shales outcropping within the Robinson Range syncline with its axis trending east-west over an approximate strike length of 30km. The BIF thicknesses are variable along strike and range from less than 50m and up to 400-500m as reported¹. The BIF’s are well represented by regional and local scale airborne magnetic images. Supergene enrichment along the BIF outcrop, producing hematite and goethite, ranges in Fe content from as low as 50% to 65% Fe (See Figure 2).

Sinosteel Midwest Group have reported three resources Raven, Raven North and Sparrow with a combined total of 9.3Mt at 56% Fe and 0.07% P. Within this the Raven North deposit is reported at 3.6Mt @ 59.03% Fe and 0.09% P. Recent success by Alchemy Resources (ASX:ALY) on 31^st May 2024 reported high grade Fe rock chips from the Valley Bore prospect located 21km to the east along the range from E52/1613.

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