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Kingsmen Reports Expanded Geochemical Data Silvia - La Plata Zones

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Vancouver, British Columbia--(Newsfile Corp. - March 3, 2025) - Kingsmen Resources Ltd. (TSXV: KNG) (OTCQB: KNGRF) ("Kingsmen" or the "Company") is pleased to report additional results from its continuing exploration program on its 100% owned Las Coloradas project, which is in the Parral mining district of the Central Mexican Silver Belt, Chihuahua Mexico.

The Silvia and La Plata zones are located on the 2,500 meter-long, NE-trending zone of structures that lies to the north of the NW-trending Soledad/Soledad II structures/vein systems. The Silvia zone is located at the intersection of the Silvia-La Plata zones and the Soledad structures/vein systems. The La Plata zone contains NE, NW and N-trending structures/veins. N-trending structures/vein systems are unusual and may, in part, be reflecting buried quartz porphyry (QP) intrusives.

The Company completed a review of the geochemistry of samples collected from the Silvia and La Plata zones to ensure maximum value is extracted from the geochemical data base in defining exploration +/- drill targets. A number of pathfinder elements vary significantly with silver. These variations are interpreted to indicate different pulses of mineralization and possibly indications of different styles of mineralization along and at depth in the two structures.

President, Scott Emerson, commented: "We have now completed geochemical sampling over our targeted zones. As previously noted on the Soledad structures and now at Silvia and Plata, the presence of high-grade samples hosted in intrusive, volcanic and sedimentary rocks confirm these are highly prospective areas for drilling in our upcoming drilling campaign."

The variation of a number of elements with silver is presented on Figures 1 to 10. Figure 1 shows silver values (previously reported) for all samples collected on the Silvia and La Plata zones. Its distribution is related to the NE-trending and NW-trending structures/vein systems. Lead (Figure 2) is more restricted in its distribution but it does track intrusive/volcanic or sediment contacts in the La Plata zone. In contrast, the zinc values more closely track the distribution of silver (Figure 3). Copper values are very low throughout but it does track silver (Figure 4). Gold values (Figure 5) indicate areas of enrichment with silver in the north-centre of La Plata, in a vein-structure zone in Silvia and in the Soledad II zone. Antimony (Figure 6), a key pathfinder element, shows a strong distribution in the central Silvia - La Plata zones where silver is weakly developed suggesting the potential for blind silver mineralization. It also tracks gold in this area. Tellurium (Figure 7) highlights intrusives/structures in south-central La Plata and in the central Silvia-La Plata zones. Bismuth tracks silver in the central Silvia-La Plata zones and in the Soledad II structure/vein system (Figure 8). Tellurium and bismuth are useful in identifying intrusion-related gold deposits. Mercury generally tracks silver, antimony, tellurium and locally gold (Figure 9). Mercury is highly mobile and often forms a halo around gold deposits. It is particularly useful in epithermal precious metal systems. Arsenic (Figure 10) has a widespread distribution that tracks silver, antimony, tellurium and gold. Arsenic is one of the most reliable pathfinder elements for precious metals. Its presence in all samples is significant.