Mr. Chris Beer reports

ATEX REPORTS FINAL PHASE VI ASSAYS EXTENDING B2B BRECCIA APPROXIMATELY 200M SOUTH IN HOLE ATXD19A; ATXD19B ENDED IN 37M OF 1.72% CUEQ

Atex Resources Inc. has released the final set of assay results for its phase VI drill program, concluding the campaign at the Valeriano copper-gold project, located in the Atacama region, Chile. Atex plans to begin its phase VII drill program shortly with more details to be provided closer to program commencement.

Drilling highlights include:

• Final phase VI drill results expanded the high-grade B2B breccia strike length approximately 200 metres to the south, where it remains open for further growth and follow-up in phase VII;
• Further defined the B2B breccia limits to the north and east and highlighted expansion potential to the north beyond B2B in mineralized rhyolite;
• New porphyry vectors were identified north and south of B2B, including porphyry-style alteration, copper mineralization and quartz veining more than 400 metres north of the known system, supporting the potential for continued exploration success beyond currently drilled areas;
• Multiple high-priority follow-up targets will be advanced in the upcoming phase VII drill program.

Key drill hole highlights are summarized in an attached table, with full technical context provided in the technical highlights section.

Chris Beer, interim president and chief executive officer, commented: "The drill results announced today continue to strengthen our understanding of the scale and geometry of the Valeriano mineralized system. At B2B, drilling has further defined the breccia geometry, demonstrated continuity at depth, expanded the known strike length to approximately 600 metres, and delivered additional higher-grade intervals of approximately 2 per cent CuEq and above. We are also seeing mineralization extend beyond the B2B breccia itself, including an approximately 150-metre true width zone of mineralized host rock to the north.

"Beyond B2B, we are encouraged by the presence of copper mineralization, strong alteration and quartz veining characteristic of porphyry systems more than 400 metres north of the known B2B zone. Combined with encouraging geological indications to the south, these results reinforce the potential for the Valeriano system to extend well beyond the areas tested to date.

"Phase VI has given us a much stronger understanding of the architecture of Valeriano and, importantly, a growing pipeline of targets for the upcoming phase VII program. We expect to provide additional details on our phase VII objectives in the near future."

Technical highlights

ATXD19A reported final intersections including 64 metres (m) of 1.01 per cent copper equivalent (CuEq) (0.66 per cent copper (Cu), 0.29 gram per tonne (g/t) gold (Au), 1.3 g/t silver (Ag) and, 103 g/t molybdenum (Mo)) from 852 m depth, and a broader interval of 228 m of 0.84 per cent CuEq (0.54 per cent Cu, 0.23 g/t Au, 1.0 g/t Ag and 129 g/t Mo) from 828 m downhole. ATXD19B was wedged from ATXD19A and drilled subparallel to it, intersecting 37 m of 1.72 per cent CuEq (0.93 per cent Cu, 0.71 g/t Au, 4.2 g/t Ag and two g/t Mo) from 1,696 m downhole and a broader interval of 446 m of 0.74 per cent CuEq (0.45 per cent Cu, 0.25 g/t Au, 1.6 g/t Ag and 23 g/t Mo) from 1,287 m downhole, and the hole ended in mineralization and remains open for follow-up:

• The hole tested the continuation of the B2B zone approximately 200 m to the south at a similar elevation, while also evaluating the continuity of the high-grade porphyry zone at depth.
• ATXD19B intersected intermineral porphyry and associated contact hydrothermal breccia, characterized by potassic alteration, chalcopyrite-dominant over bornite mineralization and intense veining toward the bottom of the hole.
• Mineralization remains open at depth and is expected to be followed up during phase VII in hole ATXD19B, which ended in mineralization grading 1.72 per cent CuEq.

ATXD25E intersected 20 m of 1.70 per cent CuEq (1.08 per cent Cu, 0.56 g/t Au, 3.1 g/t Ag and 12 g/t Mo) from 1,626 m depth, within 66 m of 1.30 per cent CuEq (0.84 per cent Cu, 0.41 g/t Au, 2.5 g/t Ag and 10 g/t Mo) from 1,590 m depth, and separately 294 m of 1.05 per cent CuEq (0.63 per cent Cu, 0.38 g/t Au, 2.5 g/t Ag and 17 g/t Mo) from 1,672 m downhole, within a broader interval of 884 m of 0.79 per cent CuEq (0.52 per cent Cu, 0.22 g/t Au, 1.6 g/t Ag and 46 g/t Mo) from 1,210 m downhole:

• This hole was designed to test the depth extent and better define the true width of the B2B zone.
• It intersected rock-milled breccia and associated intermineral porphyry, characterized by potassic alteration and copper mineralization dominated by chalcopyrite with subordinate bornite.
• The results further refine the interpreted true width of the B2B zone while extending its known limits to the east, providing additional definition of the zone's geometry and potential scale.

ATXD31B intersected 10 m of 2.22 per cent CuEq (1.36 per cent Cu, 0.79 g/t Au, 3.2 g/t Ag and three g/t Mo) from 1,894 m depth, within 118 m of 0.87 per cent CuEq (0.45 per cent Cu, 0.38 g/t Au, 1.5 g/t Ag and 6 g/t Mo) from 1,862 m depth, and separately 543 m of 0.82 per cent CuEq (0.54 per cent Cu, 0.24 g/t Au, 1.5 g/t Ag and 46 g/t Mo) from 1,303 m downhole:

• This hole was designed to test the northern and depth extensions of the B2B zone.
• It intersected a broad transition from mineralized host rock characterized by potassic alteration and chalcopyrite-dominant copper mineralization into the B2B zone, where mineralization is characterized by chalcopyrite with subordinate bornite.
• Importantly, drilling intersected a higher-grade interval of 10 m of 2.22 per cent CuEq, interpreted to represent the B2B zone and characterized by coarse chalcopyrite-dominant veining with subordinate pyrite within green-grey sericite alteration.
• The results further define the northern margin of the B2B breccia while also identifying an interpreted 150-metre true width zone of mineralized rhyolitic host rock immediately to the north, expanding the broader mineralized footprint in this direction.

ATXD31C intersected 48 m of 1.16 per cent CuEq (0.68 per cent Cu, 0.43 g/t Au, 2.2 g/t Ag and 11 g/t Mo) from 1,700 m depth and a broader interval of 528 m of 0.75 per cent CuEq (0.51 per cent Cu, 0.20 g/t Au, 1.2 g/t Ag and 55 g/t Mo) from 1,320 m downhole:

• This hole was designed to test the northeast extension of the B2B zone.
• Similar to ATXD31B, the hole intersected mineralized host rock characterized by potassic alteration and chalcopyrite-dominant mineralization with subordinate pyrite. At approximately 1,747 metres, drilling transitioned into intrusion breccias comprising rhyolite fragments within an intermineral porphyry matrix, together with metre-scale rock-milled breccia intervals. These intrusive and breccia units exhibit potassic alteration and chalcopyrite-dominant copper mineralization with subordinate bornite.
• Together with ATXD31B, the results further define the northern margin and geometry of the B2B breccia, supporting an interpreted east-west to west-northwest trend while indicating potential for continued mineralization at depth.

ATXD37 intersected 42 m of 0.50 per cent CuEq (0.39 per cent Cu, 0.06 g/t Au, 0.8 g/t Ag and 102 g/t Mo) from 1,570 m downhole:

• This hole was designed to test the northern extent of the broader porphyry system, targeting a high-velocity ambient noise tomography (ANT) anomaly beyond the currently defined B2B zone.
• It intersected mineralized rhyolite characterized by green sericite alteration overprinting a potassic alteration background, with chalcopyrite-dominant mineralization and subordinate pyrite, accompanied by A-type and B-type quartz veinlets.
• Significantly, the presence of porphyry-style alteration, mineralization and veining more than 400 metres north of the known B2B zone suggests potential proximity to a porphyry centre, either at depth or laterally, and highlights the exploration potential beyond the currently defined mineralized footprint.

ATXD39A intersected 36 m of 0.39 per cent CuEq (0.27 per cent Cu, 0.09 g/t Au, 0.6 g/t Ag and 42 g/t Mo) from 1,632 m downhole:

• This hole was designed to test the broader continuity of the porphyry system and its potential extension along the southern extent of the Valeriano system.
• The mineralized interval occurs within the rhyolitic host rock, and is characterized by pyrite with subordinate chalcopyrite mineralization, phyllic alteration overprinting a potassic alteration background and A-type quartz veinlets. Importantly, the interval includes an eight-metre rock-milled breccia zone characterized by chalcopyrite-dominant mineralization.
• While a significant portion of the hole intersected lower-grade mineralized intermineral porphyry, the occurrence of stronger mineralization immediately beyond the contact with the rhyolitic host rock provides additional geological information on the controls and distribution of mineralization along the southern extent of the Valeriano porphyry system.

Quality assurance and quality control (QA/QC)

Drill holes are collared with a PQ drill bit, reduced to HQ and, sequentially, to NQ as the drill holes progressed deeper. Drill core produced by the drill rigs was extracted from the core tubes by the drill contractor under the supervision of Atex employees, marked for consistent orientation and placed in core boxes with appropriate depth markers added. Full core boxes were then sealed before being transported by Atex personnel to the Valeriano field camp. Core at the field camp is processed, quick logged, checked for recovery, photographed and marked for specific gravity, geotechnical studies, and for assays. From camp, the core is transferred to a secure core cutting facility in Vallenar, operated by IMG, a third party consultant. Here, the core trays are weighed before being cut using a diamond saw under Atex personnel oversight. Atex geologists working at this facility double-check the selected two-metre sample intervals, placing the samples in seal bags and ensuring that the same side of the core is consistently sampled. Reference numbers are assigned to each sample and each sample is weighed. The core trays with the remaining half core are weighed and photographed. Additionally, core logs are updated, and specific gravity and geotechnical samples are collected. The remaining core is stored in racks at the company's secure facility in Vallenar.

From Vallenar samples are sent to an ALS preparation facility in Copiapo. ALS is an accredited laboratory that is independent of the company. The prepared samples were sent to the ALS assay laboratories in either Santiago, Chile, or Lima, Peru, for gold (Au-AA24), copper (Cu-AA62), molybdenum (Mo-AA62) and silver (Ag-AA62) assays, as well as and multielement ICP (inductively coupled plasma) (ME-MS61) analysis. The QA/QC program consists of insertion rates of 6 per cent for certified reference material, 2 per cent for certified blank material, and 2 per cent duplication of pulp and coarse reject material. No data quality problems were indicated by the QA/QC program.

Qualified person

Brad Ulry, PGeo, has reviewed and approved the scientific and technical information in this news release. Mr. Ulry is the chief operating officer of Dahrouge Geological Consulting Ltd., which has been retained by the company to provide geological consulting services. Mr. Ulry is a qualified person as defined by National Instrument 43-101, Standards of Disclosure for Mineral Projects, and is independent of the company for purposes of Section 1.5 of NI 43-101.

Mineral resource estimate

The mineral resource estimate for Valeriano is supported by the technical report titled "Independent Technical Report for the Valeriano Copper-Gold Project, Atacama Region, Chile" and dated Nov. 3, 2025 (with an effective date of Sept. 23, 2025), which was prepared for Atex by SRK Consulting (Canada) Inc. in accordance with NI 43-101. The Valeriano technical report is available on Atex's website.

About Atex Resources Inc.

Atex Resources is a mineral exploration company advancing its flagship Valeriano copper-gold project, located in the Atacama Region III of Chile, widely recognized as one of the world's most prospective and mining-friendly jurisdictions. The Valeriano project is emerging as one of the leading undeveloped copper assets globally and anchors an expanding, globally significant copper district. As such, it is well positioned to play an important role in meeting future demand amid increasingly constrained global copper supply. Valeriano currently has an indicated mineral resource of 475 million tonnes (t) at 0.88 per cent CuEq (0.58 per cent Cu, 0.25 g/t Au, 1.39 g/t Ag and 70.4 g/t Mo) and an inferred mineral resource of 1,511 million t at 0.75 per cent CuEq (0.50 per cent Cu, 0.20 g/t Au, 1.16 g/t Ag and 70.6 g/t Mo), as reported on Sept. 23, 2025. For further information, please visit the Atex Resources website.

We seek Safe Harbor.