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Amex Expands Central Polymetallic Zone - Drills 39.06 g/t Au, 331.92 g/t Ag, 1.14% Cu, 3.38% Zn, and 2.35% Pb over 1.30 m

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Montreal, Quebec--(Newsfile Corp. - April 8, 2025) - Amex Exploration Inc. (TSXV: AMX) (FSE: MX0) (OTCQX: AMXEF) ("Amex" or "the Company") is pleased to announce results from its ongoing drill program at the Perron Project, located in northwestern Abitibi, Quebec (see Figure 1). Today's results from PEG-25-854 have expanded the mineralized footprint of the Central Polymetallic Zone (CPZ) to the west near surface by approximately 130 m (see Figures 2-3).

CPZ Drill Results:

  • 39.06 g/t Au, 331.92 g/t Ag, 1.14% Cu, 3.38% Zn and 2.35% Pb over 1.30 m, including 48.27 g/t Au, 468.00 g/t Ag, 1.72% Cu, 4.48% Zn and 3.21% Pb over 0.80 m at a vertical depth of ~105 m - hole PEG-25-854

Jacques Trottier, PhD, Executive Chairman of Amex Exploration commented, "The Central Polymetallic Zone had not been drilled since the discovery of the High Grade Zone in late 2018, until last year's intercept of 134.36 g/t Au over 1.80 m (see November 6, 2024 Press Release), which extended the zone at depth down plunge. Today's results have extended the zone up plunge, westwards and towards surface and indicates that there is much more room for growth. As can be seen in Figure 4; by observing the gold to silver ratio, we can highlight zones of polymetallic mineralization. Our geology team has identified the potential for the extension of the CPZ to continue at depth, where there is a possible correlation with the Donna Copper Zone, found just north of the High Grade Zone. This model would match with other Volcanogenic Massive Sulfide (VMS) orebodies in the region such as the historical Normétal Mine, which was zinc-rich close to surface and more copper-rich at depth."

Central Polymetallic Zone

The CPZ is interpreted as a discordant linear volcanogenic hydrothermal feeder crosscut by gold bearing quartz-sulfide veins. The quartz-sulfide veins observed in PEG-25-854 (see Figure 5) are interpreted as syn-tectonic. The gold-rich veins are mineralized in chalcopyrite, sphalerite, pyrite, pyrrhotite, and galena. Silver values being almost ten times higher than gold is very typical of the CPZ. Higher gold grades are related to higher sulphide contents and are correlative either with zinc or copper values.

Since closing of the database on June 30, 2024 for the Mineral Resource Estimate and the Preliminary Economic Assessment, subsequent drilling has successfully intercepted both the up and down plunge extensions of the CPZ zone. PEG-25-854 has unlocked CPZ mineralization close to surface towards the west, while PE-24-801 found the potential downwards extension of the zone to the east (see November 6, 2024 Press Release).