VR Resources Confirms PGE and Nickel-Copper Fertility at Empire Project in Northwest Ontario

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VR Resources Ltd.
VR Resources Ltd.

VANCOUVER, British Columbia, Feb. 26, 2025 (GLOBE NEWSWIRE) -- VR Resources Ltd. (TSX.V: VRR, FSE: 5VR; OTCBB: VRRCF), the "Company", or “VR”, announces results from the maiden reconnaissance drill program on the Westwood Target, part of the Empire Project in Northwestern Ontario.

Copper, nickel and platinum group elements (PGE) mineralization within the Westwood complex was first observed at the Trans Canada highway occurrence on the western margin of a more than 2 km long, northeast striking magnetic high anomaly. Drilling has now confirmed the anomaly to be a fertile, multiphase mafic-ultramafic intrusion with magmatic cumulate textures and sulfide segregation spanning more than 900m, on opposing sides of the intrusion (Figure 1). The highway occurrence shows a southeasterly dip to the zonation within the intrusive complex, which is also now observed in oriented drill core measurements; the northern margin of the anomaly is now inferred to be the basal contact of the multi-phase and steeply dipping intrusion and is considered the most prospective for PGE.

Highlights of the recent drilling include:

  • 1m intervals with 262, 138 and 118 ppb Pd+Pt on the basal contact in Holes 4 and 5, from the same pad, in weakly developed segregation textures, along trend from the highway outcrop; see core in Photo 1.

  • Copper-nickel mineralization up to 0.09% Cu and 0.11% Ni, with anomalous PGE, at 320m depth in Hole 2;

  • Evidence for localized sulfide saturation and Ni-Cu-PGE depletion, movement and enrichment within cumulate textured mafic rocks across the complex.

From VR Resource’s CEO, Justin Daley: “The full dataset for drilling geochemistry has shown us that the right processes are at play for Ni-Cu-PGE mineralization within the Westwood intrusive complex, and perhaps within each of the nearby targets in our district-scale Empire project. As such, this drilling is an important step in advancing our exploration model for fertile intrusions in this previously unexplored part of the Marmion terrane.

The text in the following sections describes the two specific styles of sulfide mineralization intersected on opposing sides of the complex. The prospectivity along the northern contact of the intrusion, with anomalous PGEs, highlights potential for further precious metals mineralization (Au-Pt-Pd) along this magnetic gradient trend, particularly at other DIGHEM anomalies.

It is also encouraging to see a strong spatial relationship between copper-nickel sulfide mineralization in Hole 2 and the DIGHEM and IP chargeability anomaly targeted by that hole. The down-hole EM probe completed on Hole 002 further refines this correlation which is evident in the cross-section in Figure 1.