공시 • Jun 09
Canadian GoldCamps Corp. Receives New Gold Analytical Results From High-Resolution Re-Sampling Program At Mercator Gold Project
Canadian GoldCamps Corp. announced the receipt of new gold analytical results from a high-resolution re-sampling program completed on drill core and mineralized material from the Company’s flagship Mercator Gold Project in the Caniapiscau district of northeastern Québec. The 25 cm re-sampling program has provided a more detailed view of gold distribution within the Mercator system. Of the 111 individual samples collected from previously identified mineralized intervals, approximately 82% returned gold values above detection limits, supporting the continuity of mineralization across the intervals tested, demonstrating the widespread distribution and continuity of gold mineralization within the horizons tested. The program also identified additional higher-grade intervals that are currently undergoing verification and confirmatory analytical work. Results from this ongoing review are expected to be reported in a subsequent news release. The data generated through this program will help refine exploration targeting and support the next phase of work at the Mercator Gold Project. The program consisted of 111 sub-samples cut at 25 cm intervals from previously mineralized intervals in drill holes MCT-22-08, MCT-22-11 and MCT-22-03, as well as from three additional mineralized zones currently under characterization (identified internally as Zones Unid-1, Unid-2 and Unid-3). All samples were analyzed by Impact Geosciences (IGS) in Delson, Québec using Pb-Fusion Fire Assay with ICP-OES finish (RDL 0.006 ppm Au). The results further support the interpretation of a stratiform gold system hosted within granulite-facies silicate-sulphide banded iron formations (BIFs) of the Meridian Zone. Drill Hole Collar Locations, Orientations and Re-Sampled Interval Depths: MCT-22-08, Easting 457,469, Northing 5,875,099, Collar Elev. 730, Azimuth 146°, Dip -47°, Hole Length 186.0 m, Re-Sampled Interval 47.15 – 64.95 m, Reported Composite Grade 2.62 g/t Au over 17.80 m; MCT-22-11, Easting 457,512, Northing 5,875,271, Collar Elev. 743, Azimuth 150°, Dip -45°, Hole Length 272.7 m, Re-Sampled Interval 99.00 – 108.00 m, Reported Composite Grade 1.02 g/t Au over 9.00 m; MCT-22-11, Re-Sampled Interval 151.25 – 155.50 m, Reported Composite Grade 1.24 g/t Au over 4.25 m; MCT-22-11, Re-Sampled Interval 184.20 – 193.50 m, Reported Composite Grade 1.19 g/t Au over 9.30 m; MCT-22-03, Easting 458,330, Northing 5,875,443, Collar Elev. 798, Azimuth 150°, Dip -60°, Hole Length 102.0 m, Re-Sampled Interval 26.85 – 35.50 m, Reported Composite Grade 1.22 g/t Au over 8.65 m; MCT-22-03, Re-Sampled Interval 40.75 – 42.20 m, Reported Composite Grade 1.43 g/t Au over 1.45 m. Collar coordinates are reported in NAD83 /UTM Zone 19N (EPSG:26919); collar elevations (Z) are metres above sea level. Azimuth and dip describe the orientation of each drill hole at the collar. Re-sampled intervals are downhole sample-interval depths (metres) measured from the collar; the 25 cm sub-samples reported in this release were cut within these intervals. Reported composite grades are the previously disclosed weighted-mean gold grades over the mineralized intervals subsequently re-sampled at 25 cm support. Reported interval lengths are downhole core lengths; true widths are not known. Collar, survey and interval data are sourced from the Stelmine Canada Ltée drill database transmitted to MRNF/SIGÉOM (22 March 2024). Highlights of the 25 cm Re-Sampling Program: Approximately 82% of the 111 high-resolution samples returned gold values above detection limits, supporting the continuity of mineralization across multiple drill intercepts and target zones. Drill hole MCT-22-11: Sub-sampling returned 6.77 g/t Au (sample 22-011-14) and 6.30 g/t Au (sample 22-011-27); 16 of 35 sub-samples returned = 1.0 g/t Au, confirming the sustained high-grade nature of this intersection. Drill hole MCT-22-08: Sub-sampling returned 3.40 g/t Au (sample 22-008-06), 3.22 g/t Au (sample 22-008-21) and 2.93 g/t Au (sample 22-008-22); 11 of 25 sub-samples returned = 1.0 g/t Au, with the 25 cm resolution successfully isolating individual high-grade bands within the broader 17.80 m mineralized envelope previously reported (2.62 g/t Au). Drill hole MCT-22-03: 5 of 19 sub-samples returned = 1.0 g/t Au, with a peak value of 1.48 g/t Au (sample 22-003-8). Zones Unid-1, Unid-2 and Unid-3: Out of 30 sub-samples, 19 returned = 1.0 g/t Au, with 6 sub-samples exceeding 2.0 g/t Gold, establishing these zones as priority targets for follow-up work during the 2026 field season. Strong reproducibility: Laboratory replicate analysis of the highest sub-sample (22-011-14) returned 6.77 g/t Au and 6.99 g/t Au on independent aliquots, demonstrating excellent intra-sample homogeneity at the 25 cm scale. Quality assurance: All Certified Reference Materials (Oreas 236, certified at 1.85 ppm Au) returned recoveries between 0.978 and 1.054 of expected value (within 1–2 s); all blanks returned values below the reportable detection limit. Multi-element data pending: Additional analytical work covering arsenic, copper, sulphur and the full pathfinder suite (As, Cu, Fe2O3, MnO, S, ± PGE) is in progress and will be reported in a subsequent news release. Geological Setting: Mercator’s Granulite-Facies BIF System. The Mercator Property is positioned in the southeastern Churchill Province of the Canadian Shield, in the Caniapiscau district of northeastern Québec, approximately 170 km west of Fermont. The property covers 113 mineral claims (˜58.6 km²) along a regional NE-trending metasedimentary belt characterized by strong magnetic and electromagnetic responses attributed to iron-rich metasediments and silicate-sulphide-bearing banded iron formations (BIFs) metamorphosed to the granulite facies. Gold mineralization at Mercator is hosted within stratiform silicate-sulphide BIF horizons intercalated with paragneiss, pyroxene-bearing gneiss and minor mafic intrusive units. These iron formations consist of finely banded layers of (i) quartz ± chert; (ii) garnet-pyroxene assemblages dominated by iron-rich ferrosilite (orthopyroxene) and hedenbergite (clinopyroxene); and (iii) pyroxene-sulphide layers carrying variable proportions of pyrrhotite (typically 1–65 vol.%), arsenopyrite, löllingite, pyrite and chalcopyrite.