Sable Samples up to 4.38% Cu, 140 g/t Au, and 584 g/t Ag in Preliminary Sampling Program at the Zorro Project, San Juan, Argentina
VANCOUVER, British Columbia, Jan. 22, 2026 (GLOBE NEWSWIRE) -- Sable Resources Ltd. ("Sable" or the "Company") (TSXV:SAE | OTCQB:SBLRF) is pleased to announce that it has received results for 55 out of a total of 98 rock samples collected during a preliminary review of its recently acquired Zorro Project in San Juan, Argentina (see Sable’s news release dated January 15, 2026).
This initial review was focused on some of the historic artisanal mining occurrences located around the 7km by 4km Zorro magnetic anomaly. Sample results returned highly encouraging values of Cu, Ag and Au (with associated Pb, and Zn), within three distinct areas of the property. Notably, however, most of the Zorro property remains completely unexplored.
Of the 55 sample results received, 19 samples returned values higher than 0.1% Cu with maximum values of 4.38% Cu; 19 samples returned values greater than 1 g/t Au with maximum values of 140.5 g/t Au; 19 samples returned values greater than 10 g/t Ag reaching maximum values of 584 g/t Ag. In addition, 18 samples returned values over 0.1% Pb.

Figure 1. Values of Cu (left) and Au (right) showing the location of the three current target zones.
The observed mineralization styles, and apparent geochemical/alteration associations and zoning define three separate, aerially significant target areas (Figure 1):
Zorro Copper
The Zorro Copper target area is well defined within a zone of approximately 650m by 500m. Sampling returned multiple values grading >0.1% Cu, and up to 4.38% Cu (Figure 2 and Table 1). Observed mineralization consists of sheeted quartz-carbonate veins and veinlets containing chalcopyrite, hematite and magnetite, hosted within Permian granite (Figure 3). In addition to Cu, sampling returned significant Ag values, up to 114 g/t Ag. Silver appears broadly correlative with Cu, with 73% of the Zorro Copper samples returning greater than 5 g/t Ag. Furthermore, and importantly, Au values, although less consistent, ranged from <0.1 g/t up to 15.3 g/t Au, with six samples returning >0.1g/t Au (Figure 2 and Table 1). Typical of Intrusion-Related mineralization, Bi, Te, and W are anomalous, and in this case, generally correlative with Au values. Sable’s next steps will include detailed mapping and sampling of this large-scale, outcropping Cu (Ag, Au) system.

Figure 2. Detail of the Zorro Cu zone showing Cu values in percentage for samples received.
Zorro Veins
Located northeast of the Zorro Copper zone, the Zorro Veins zone comprises a series of quartz-carbonate-pyrite veins that have been historically exploited in artisanal mine workings. Sable’s sampling program returned high-grade values up to 140 g/t Au and 584 g/t Ag, including 7 samples that returned >5g/t Au (Figure 1, Table 1). The sulphide mineralogy of the veins includes galena (one sample reported >20% Pb), sphalerite, local chalcopyrite and arsenopyrite. Sable’s geology team considers the vein system to be of intermediate-sulphidation epithermal nature. Sable will conduct detailed mapping and further sampling of the veins to define their distribution, continuity, grade, and depth potential, as well as to ascertain their significance as geochemical vectors to non-outcropping mineralization in the vicinity.

Figure 3. A and B: Examples of chalcopyrite-rich quartz-carbonate veins from the Zorro Cu target. Note the particularly coarse-grained chalcopyrite crystals. C: Sheeted veining and local stockwork characteristic of structural corridors at Zorro Cu. The host granite is intensely altered with Fe-Carbonate within the veining zones.
Zorro Bx
The Zorro Bx zone outcrops 900 metres east of the Zorro Copper target. It represents a high-level magmatic-hydrothermal breccia, containing clasts of sedimentary country rock with quartz-sericite-pyrite cement. Samples collected from the breccia returned well defined epithermal pathfinder element anomalies, including for As, Ba, Mn, Sb, with lesser anomalies for Mo, and Pb. Additional geological and alteration mapping, sampling and geophysical surveys will be used to study the Zorro Bx zone, and to determine its possible transition to Cu and/or Au-Ag mineralization at depth.
Dr. Ruben Padilla, President and CEO of Sable, commented, “We are highly encouraged by this set of initial results. The widespread nature and variability of mineralization and alteration observed at the Zorro Project speaks to its potential to host bulk-tonnage Cu (Ag, Au) deposits (e.g. Zorro Copper) and high-grade Au-Ag (Pb, Zn) deposits (e.g. Zorro Veins). In addition, geochemical and alteration anomalies such as at Zorro Bx can occur peripheral to or above significant porphyry-style Cu or epithermal Au-Ag occurrences. The Zorro Copper zone provides us with a clear fast-track diamond drill target, given the size and strong Cu-Ag-rich signature of outcropping mineralization. Sable’s geology team is advancing detailed surface work at all the above outlined targets, in parallel with widespread prospecting in other areas of this under-explored property. Our work will be greatly facilitated by the ease of access and all-weather altitude (2,600masl) of the project area, which will allow us to advance exploration year round.”
Table 1. Location and results for highlighted samples with values greater than 0.1% Cu, 0.1 g/t Au, 5 g/t Ag, and 0.1% Pb and Zn.
| Sample | Grid | North | East | Elevation | Site | Cu % | Au (g/t) | Ag (g/t) | Pb % | Zn % |
| E43077 | WGS 84 / UTM zone 19S | 6626602 | 453836 | 2790 | Outcrop | 4.38 | 0.128 | 16.7 | 0.0124 | 0.0048 |
| E43011 | WGS 84 / UTM zone 19S | 6626828 | 453982 | 2747 | Dump | 2.94 | 3.24 | 74.4 | 0.017 | 0.0036 |
| E43034 | WGS 84 / UTM zone 19S | 6626903 | 453807 | 2774 | Outcrop | 2.46 | 0.404 | 18 | 0.0284 | 0.0023 |
| E43030 | WGS 84 / UTM zone 19S | 6627115 | 453875 | 2748 | Outcrop | 2.29 | 0.112 | 7.02 | 0.00725 | 0.0018 |
| E43035 | WGS 84 / UTM zone 19S | 6627249 | 454010 | 2740 | Outcrop | 1.44 | 1.045 | 8.13 | 0.00075 | 0.003 |
| E43010 | WGS 84 / UTM zone 19S | 6626827 | 453974 | 2746 | Dump | 0.742 | 2.35 | 4.8 | 0.00424 | 0.0028 |
| E43012 | WGS 84 / UTM zone 19S | 6626771 | 453943 | 2758 | Outcrop | 0.67 | 0.058 | 2.91 | 0.011 | 0.0023 |
| E43009 | WGS 84 / UTM zone 19S | 6627792 | 454314 | 2690 | Float | 0.538 | 1.02 | 24.2 | 0.1405 | 0.0069 |
| E43031 | WGS 84 / UTM zone 19S | 6627052 | 453823 | 2759 | Outcrop | 0.535 | 0.017 | 7.99 | 0.00296 | 0.0033 |
| E43044 | WGS 84 / UTM zone 19S | 6627162 | 453518 | 2784 | Float | 0.487 | 0.013 | 10.4 | 0.00129 | 0.0109 |
| E43032 | WGS 84 / UTM zone 19S | 6626843 | 453617 | 2806 | Outcrop | 0.381 | 0.02 | 11.15 | 0.0019 | 0.0022 |
| E43014 | WGS 84 / UTM zone 19S | 6626703 | 453676 | 2792 | Outcrop | 0.306 | 0.027 | 7.19 | 0.00964 | 0.0008 |
| E43041 | WGS 84 / UTM zone 19S | 6627171 | 453586 | 2781 | Outcrop | 0.208 | 0.014 | 5.48 | 0.0006 | 0.0055 |
| E43036 | WGS 84 / UTM zone 19S | 6626872 | 453601 | 2807 | Outcrop | 0.1965 | 0.007 | 2.53 | 0.00056 | 0.0034 |
| E43079 | WGS 84 / UTM zone 19S | 6625671 | 452290 | 3107 | Dump | 0.1725 | 1.105 | 238 | 17.35 | 0.151 |
| E43029 | WGS 84 / UTM zone 19S | 6627122 | 453917 | 2738 | Outcrop | 0.1535 | 0.006 | 1.83 | 0.00089 | 0.0025 |
| E43043 | WGS 84 / UTM zone 19S | 6627702 | 453731 | 2760 | Outcrop | 0.1515 | 0.014 | 1.88 | 0.00079 | 0.0037 |
| E43024 | WGS 84 / UTM zone 19S | 6627599 | 454844 | 2665 | Dump | 0.148 | 2.73 | 139 | 10 | 1.565 |
| E43021 | WGS 84 / UTM zone 19S | 6627198 | 454080 | 2711 | Outcrop | 0.11 | 15.3 | 117 | 0.565 | 0.196 |
| E43003 | WGS 84 / UTM zone 19S | 6627890 | 455209 | 2708 | Dump | 0.0947 | 34.7 | 25.1 | 2.84 | 0.426 |
| E43037 | WGS 84 / UTM zone 19S | 6626612 | 453338 | 2848 | Outcrop | 0.0918 | 0.007 | 0.41 | 0.00036 | 0.0027 |
| E43006 | WGS 84 / UTM zone 19S | 6627775 | 454615 | 2714 | Outcrop | 0.0797 | 1.4 | 584 | 20 | 0.923 |
| E43005 | WGS 84 / UTM zone 19S | 6627671 | 454578 | 2684 | Dump | 0.0757 | 3.01 | 35.8 | 0.0849 | 0.0078 |
| E43008 | WGS 84 / UTM zone 19S | 6627875 | 454415 | 2693 | Dump | 0.0682 | 6.32 | 7.61 | 0.0763 | 0.0345 |
| E43002 | WGS 84 / UTM zone 19S | 6627618 | 455240 | 2670 | Outcrop | 0.0617 | 5.83 | 123 | 2.89 | 0.367 |
| E43078 | WGS 84 / UTM zone 19S | 6626255 | 453271 | 2851 | Subcrop | 0.0553 | 0.229 | 11.15 | 1.585 | 0.167 |
| E43076 | WGS 84 / UTM zone 19S | 6628281 | 454913 | 2831 | Outcrop | 0.0544 | 13.3 | 15.25 | 0.1125 | 0.184 |
| E43049 | WGS 84 / UTM zone 19S | 6628565 | 454963 | 2705 | Dump | 0.0493 | 7.01 | 109 | 3.9 | 0.176 |
| E43004 | WGS 84 / UTM zone 19S | 6627747 | 455066 | 2709 | Dump | 0.0465 | 2.9 | 6.39 | 0.143 | 0.1415 |
| E43050 | WGS 84 / UTM zone 19S | 6628569 | 454962 | 2703 | Outcrop | 0.0322 | 3.07 | 42.8 | 1.785 | 0.765 |
| E43015 | WGS 84 / UTM zone 19S | 6626153 | 453465 | 2874 | Outcrop | 0.0285 | 0.005 | 0.65 | 0.00602 | 0.0088 |
| E43023 | WGS 84 / UTM zone 19S | 6627604 | 454835 | 2665 | Outcrop | 0.0283 | 1.595 | 9.14 | 0.257 | 0.757 |
| E43045 | WGS 84 / UTM zone 19S | 6628690 | 454973 | 2695 | Dump | 0.0281 | 1.855 | 26.3 | 1.43 | 0.286 |
| E43047 | WGS 84 / UTM zone 19S | 6628658 | 454953 | 2705 | Outcrop | 0.0279 | 0.762 | 4.7 | 0.1445 | 0.552 |
| E43025 | WGS 84 / UTM zone 19S | 6627557 | 454845 | 2658 | Dump | 0.0211 | 0.027 | 1.5 | 0.0191 | 0.0385 |
| E43038 | WGS 84 / UTM zone 19S | 6626618 | 453059 | 2892 | Outcrop | 0.0178 | 0.006 | 0.49 | 0.0005 | 0.0055 |
| E43046 | WGS 84 / UTM zone 19S | 6628668 | 454958 | 2704 | Dump | 0.0174 | 140.5 | 259 | 9.99 | 0.0493 |
| E43001 | WGS 84 / UTM zone 19S | 6627622 | 455242 | 2680 | Outcrop | 0.016 | 0.749 | 4.27 | 0.19 | 0.1745 |
SAMPLE PREPARATION AND QA/QC
Sample preparation for projects in Argentina is carried out by ALS Minerals, at its facility located in Mendoza with analyses carried out at their laboratory in Lima, Peru. Sample preparation includes drying in an oven at a maximum temperature of 60°C, fine crushing of the sample to at least 70% passing less than 2 mm, sample splitting using a riffle splitter, and pulverizing a 250 g split to at least 85% passing 75 microns (code PREP-31). The samples contained in this news release were analyzed by methods Au-AA24 (Fire Assay Fusion and Atomic Absorption Spectrometry finish) and ME-MS61 (Four Acid Digestion with Mass Spectrometry finish), the latter includes 48 elements (Al, Ag, As, Ba, Be, Bi, Ca, Cd, Ce, Co, Cr, Cs, Cu, Fe, Ga, Ge, Hf, In, K, La, Li, Mg, Mn, Mo, Na, Nb, Ni, P, Pb, Rb, Re, S, Sb, Sc, Se, Sn, Sr, Ta, Te, Th, Ti, Tl, U, V, W, Y, Zn, Zr). Both digestion methods dissolve most minerals but not all elements are quantitatively extracted in some sample matrices. ALS additionally collects a subsample from the coarse reject to be analyzed by Terraspec with spectral data sent to AISIRIS Australia to be processed and interpreted.
Control samples (standards, blanks, and duplicates) are inserted systematically, and their results evaluated according to the Company protocols.
QUALIFIED PERSON
Luis Arteaga M.Sc. P.Geo., Vice President Exploration, is the Company's Qualified Person as defined by NI 43-101. He has reviewed and approved the technical information in this news release.
ABOUT THE ZORRO PROJECT
The Zorro Project has been recently consolidated by Sable through signing of an option agreement and ground staking, with a total 5,236-hectare land package. The project is located on the Frontal Cordillera of San Juan, directly north of the Minsud/South32 Chita Valley Project which includes two copper and polymetallic deposits: the Chinchillones deposit1 containing indicated resources of 188 Mt @ 0.41% CuEq (0.25% Cu, 0.11 g/t Au, 10.6 g/t Ag, 36 ppm Mo, 0.16% Zn) and inferred resources of 573 Mt @ 0.36% CuEq (0.22% Cu, 0.09 g/t Au, 9.0 g/t Ag, 93 ppm Mo, 0.11% Zn); and the Chita South Porphyry Deposit1 containing indicated resources of 33.1 Mt @ 0.43% Cu and inferred resources of 8.6 Mt @ 0.40% Cu. Sable’s Don Julio Project which includes four active porphyry targets (Gringa, Morro, Punta Cana, and Tocota) is located 21km west of Zorro.
Potential of the Zorro Project was recognized through Sable’s regional target generation work. The project contains a number of historical mineral occurrences and workings surrounding a large magnetic anomaly of about 7km by 4km that seems to be caused by a diorite stock which intrudes Carboniferous sediments and Permo-Triassic granites.
ABOUT SABLE RESOURCES LTD.
Sable is a well-funded junior grassroots explorer focused on the discovery of Tier-One new precious metal and copper projects through systematic exploration in endowed terranes located in favorable, established mining jurisdictions. Sable’s focus is developing its large portfolio of new Greenfields projects to resource level. Sable is actively exploring the San Juan Regional Program (163,969 ha) incorporating the Don Julio, El Fierro, Cerro Negro, and Zorro projects in San Juan province, Argentina and the Copper Queen (15,133 ha), Copper Prince (3,980 ha), and Core Mountain (1,925 ha) properties in British Columbia.
For further information, please contact:
Ruben Padilla, President & CEO at ruben.padilla@sableresources.com or +1 (520) 488-2520
Related link: sableresources.com
Neither the TSX Venture Exchange nor its Regulation Services Provider, as that term is defined in the policies of the TSX Venture Exchange, accepts responsibility for the adequacy or accuracy of this release.
CAUTION REGARDING FORWARD-LOOKING STATEMENTS
Certain statements contained in this press release constitute forward-looking information. These statements relate to future events or future performance. The use of any of the words "could", "intend", "expect", "believe", "will", "projected", "estimated" and similar expressions and statements relating to matters that are not historical facts are intended to identify forward-looking information and are based on Sable’s current belief or assumptions as to the outcome and timing of such future events. Actual future results may differ materially. Although such statements are based on reasonable assumptions of Sable’s management, there can be no assurance that any conclusions or forecasts will prove to be accurate.
While Sable considers these assumptions to be reasonable based on information currently available, they may prove to be incorrect. Forward-looking information involves known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements to be materially different from any future results, performance or achievements expressed or implied by the forward-looking information. Such factors include risks inherent in the exploration and development of mineral deposits, including risks relating to changes in project parameters as plans continue to be redefined, risks relating to variations in grade or recovery rates, risks relating to changes in mineral prices and the worldwide demand for and supply of minerals, risks related to increased competition and current global financial conditions, access and supply risks, reliance on key personnel, operational risks, and regulatory risks, including risks relating to the acquisition of the necessary licenses and permits, financing, capitalization and liquidity risks.
The forward-looking information contained in this release is made as of the date hereof, and Sable is not obligated to update or revise any forward-looking information, whether as a result of new information, future events or otherwise, except as required by applicable securities laws. Because of the risks, uncertainties and assumptions contained herein, investors should not place undue reliance on forward-looking information. The foregoing statements expressly qualify any forward-looking information contained herein.
1 Mineral Resources Data from the Chita Valley Project was obtained from Minsud Resources Corp.’s website – www.minsud.com
Figure 1.
Values of Cu (left) and Au (right) showing the location of the three current target zones.
Figure 2.
Detail of the Zorro Cu zone showing Cu values in percentage for samples received.
Figure 3.
A and B: Examples of chalcopyrite-rich quartz-carbonate veins from the Zorro Cu target. Note the particularly coarse-grained chalcopyrite crystals. C: Sheeted veining and local stockwork characteristic of structural corridors at Zorro Cu. The host granite is intensely altered with Fe-Carbonate within the veining zones.
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