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VIZSLA COPPER STRENGTHENS PORPHYRY POTENTIAL AT POPLAR SOUTH: IDENTIFIES STRONG IP CHARGEABILITY ANOMALY

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VANCOUVER, BC, Jan. 15, 2025 /CNW/ - Vizsla Copper Corp. (TSXV: VCU) (OTCQB: VCUFF) (FRANKFURT: 97E0) ("Vizsla Copper" or the "Company") is pleased to report results from a recently completed induced polarization (IP) survey across parts of the Poplar South target at the Poplar project (the "Project" or "Poplar") in northwest British Columbia (Figure 1). The Poplar project also hosts the porphyry-related Poplar copper and gold deposit (Table 1).

HIGHLIGHTS

  • New chargeability and resistivity data support the strong prospectivity for porphyry-related mineralization at Poplar South

  • Key chargeability and resistivity anomalies are coincident with other geophysical and geochemical anomalies  and represent high-priority drill targets

  • Thin veneer of glacial till across the highest priority target areas may have hidden mineralization from previous operators

"With the completion of this IP survey we now have the final dataset required to refine our exploration model for the Poplar South target," commented Steve Blower, Vice President of Exploration. "The presence of overlapping geological, geochemical and geophysical anomalies strongly supports the high-prospectivity for porphyry-related mineralization across this area. We are currently designing a robust drill program to systematically test the Poplar South target in the first half of 2025." 

The Poplar South IP Survey

The 2024 Poplar South IP survey consisted of over 20 line kilometers across 9 survey lines spaced 200 meters apart. The survey was designed to characterize and detect subsurface sulfide mineralization associated with pronounced coincident geophysical (magnetic and EM) and multi-element soil-geochemical anomalies at the Poplar South target area (Figure 1)

At surface, the Poplar South target is characterized by a broad, ~8 by 2 kilometer zone of quartz-sericite-pyrite (phyllic) alteration observed along local road-cuts and sparse outcrop on ridges (Figure 2, see News Release dated August 12, 2024). Zones of strong epidote-chlorite-magnetite alteration locally crop out near the valley bottom, proximal to the strongest geochemical and geophysical anomalies. Recently completed airborne geophysical surveys (MobileMT and high-resolution magnetics) outlined a complex, kilometer-scale conductivity-high cored by a lower-conductivity (high-resistivity) zone associated with a circular magnetic-low (Figure 2). This area is also associated with a moderate chargeability response that increases with depth towards a >50 m/v anomaly (Figure 4). These geophysical anomalies are mutually coincident with an open-ended, ~1,200 by 800 meter, multi-element (copper-molybdenum-silver) soil geochemical anomaly (see News Release dated October 8th, 2024 and Figure 3). A historical shallow drill hole completed in 1995, near the margins of the strongest coincident anomalies, returned  67.1 meters of 0.18% copper (drill hole 95-05, Figure 4)2. The percussion drill hole reportedly intersected potassically altered intrusive rocks with quartz-chalcopyrite-molybdenite mineralization throughout its length. The new 3D chargeability model suggests that hole 95-05 was terminated too early and the Poplar South target should be explored at depth (Figure 4).