Alpha Exploration Announces Additional New Drill Results from the Aburna Gold District, Kerkasha Project, Eritrea

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Calgary, Alberta--(Newsfile Corp. - January 9, 2025) - Alpha Exploration Ltd. (TSXV: ALEX) ("Alpha" or the "Company") announces additional drill results from its 7,868m drill program at the Aburna orogenic gold prospect within its 100% owned, 771 km² Kerkasha Project located in Eritrea.

Aburna is a major, district scale orogenic gold project that, based on surface geochemistry, extends over an area of at least 7km long and 2km wide and is one of three significant discoveries made by Alpha on the Kerkasha licence to date. Exploration to date at Aburna has defined six primary areas of interest including the Hill 52 and Central prospects (see Figure 1, below). This newly released data is from drillholes in the Hill 52/Central prospect area, now termed the Central Aburna Antiform (CAA).

Assays from 25 additional drillholes completed in July 2024 have now been received. Alpha is pleased to report assays from both the Hill 52 and Central areas which support current thinking on the macroscopic structural controls of gold mineralization at Aburna.

HIGHLIGHTS:

  • From Hill 52 Prospect:

    • 6m @ 2.29 g/t gold (ABRD136)

    • 6m @ 2.97 g/t gold (ABR140)

    • 4m @ 2.26 g/t gold (ABR151)

    • 6m @ 4.98 g/t gold (ABR154)

    • 4m @ 2.00 g/t gold (ABR155)

  • Mineralization in the Central Aburna Antiform (CAA) is conformable to the current macro-structural gold mineralization controls.

Hill 52/ Central Prospects or the Central Aburna Antiform (CAA)

Drillhole collar information from the 25 drillholes covered by this press release are shown in Table 1, while Table 2 shows the significant intervals from these 25 drillholes. All mineralized intervals intersected occurred within the macro-structural zones targeted, supporting the current mineralization-control model.

Drillholes ABRD136, ABRD137, ABRD138, ABR139, ABR145, ABR146, ABR147, ABR148, ABR149 and ABR152 targeted a potential reverse fault which, it is proposed, fractures the axial crest of the Central Aburna Antiform or CAA. After a macro-structural simulation and cross-sectional review, it has become apparent that mineralization at the CAA occurs in two such 'preparation' zones; one conformable with the regional foliation along the hinge-zone of the antiform and the other being a more passively fractured lithological unit, called the Hill 52 Unit (Hronsky, 2024), sandwiched between the upper and lower chlorite schists. These two units are more ductile than adjacent lithologies, creating a rheologic difference.

The axial crest reverse fault appears to have formed parallel to a major stepover fault between the Tocina and Aburna shear zones on the southeastern margin of the CAA. It is postulated that the stepover fault itself became "locked-up", with energy forcing a wrench rotational disruption along the axial crest of the CAA creating the axial crest reverse fault. This potential reverse fault appears to extend for approximately 800m from the southwest end of the Hill 52 prospect to the northeast end of the Central prospect, all now termed the Central Aburna Antiform or CAA. Gold mineralization along the length of the reverse fault occurs within a zone which varies from 60m to 120m wide and is open to the northeast, southwest and down dip.