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VR Resources Identifies Geochemical Trends from New Data on Copper-Gold Veins at Silverback Project, Ontario

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VR Resources Ltd.
VR Resources Ltd.

VANCOUVER, British Columbia, April 08, 2025 (GLOBE NEWSWIRE) -- VR Resources Ltd. (TSX.V: VRR, FSE: 5VR; OTCBB: VRRCF), the "Company", or “VR”, is pleased to announce new data, and results of a comprehensive geochemical study, at its 100%-owned Silverback Project (or “Silverback”) in Northwest Ontario, based on core samples from the two scout drill programs across three key target areas known as West Dyke (WD), Central Zone (CZ) and North Arm (NA).

  • The new data reveal clear vectors along a dominant northeasterly structural corridor that correlates with anomalous gold zones, and highlight numerous, high-priority and untested zones for follow-up exploration.

Methods
Analysis of base metals and trace elements in epizonal, intrusion-associated mineral systems help to vector along, and map, gold pathways across the project area. By normalizing vector element concentrations such as arsenic (As), antimony (Sb), bismuth (Bi), molybdenum (Mo) and tungsten (W) against titanium (Ti), a stable reference element unaffected by hydrothermal alteration, the analysis eliminates background noise from Silverback’s mixed mafic-felsic volcanic and porphyry intrusive rocks, revealing important trends. These relationships and trends can then be used to plan property-scale till sampling.

Key geochemical indicators include:

  • Up to 0.34% copper and 2.6 g/t silver were observed alongside 65 ppb gold in a quartz-sulfide vein at the NA target (Photo 1), located 1.5 km from the main surface showing in the center of the property, on the same structural trend.

  • Each drill target has elevated arsenic over antimony (As/Sb) and anomalous gold on the strongest shear zones, indicating the northeast structures are localizing and concentrating the gold-bearing fluids (Figure 1).

  • Tungsten over molybdenum (W/Mo) ratios increase considerably toward the southwest, which is a strong vector for cooler, gold-bearing fluids around the WD target in the southwest part of the property where the highest gold values found in drilling to date are in Hole 2 (Figure 2).

Picture1
Picture1


Photo 1. Copper, silver and gold mineralization in quartz veining from Hole 8 located at the 6-channel EM anomaly from a 1980’s OGS survey that is coincident with a DIGHEM conductivity anomaly from VR’s 2023 survey (Figure 1). The pyrite-chalcopyrite quartz vein carries 0.34% copper, 2.6 gpt silver and 65 ppb gold, with similar mineralization styles and metal ratios as the main surface showing located approximately 1.5 km along structural trend to the southwest.

Drill holes and sample coverage across the target areas are widely spaced, leaving considerable room for discovery of a new mineral system. In addition to the gold-bearing trend already identified, numerous untested DIGHEM conductors and shallow IP anomalies occur along the northeast-trending structural corridors which are interpreted to be key controls on fluid flow and mineralization.