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VIZSLA COPPER IDENTIFIES A BROAD IP CHARGEABILITY ANOMALY AT THE GREAT PLAINS TARGET AREA, WOODJAM PROJECT

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VANCOUVER, BC, Oct. 30, 2024 /CNW/ - Vizsla Copper Corp. (TSXV: VCU) (OTCQB: VCUFF) (FRANKFURT: 97E0) ("Vizsla Copper" or the "Company") is pleased to report results from a direct current induced polarization (DCIP) survey within the Great Plains target area at the Woodjam project (the "Project" or "Woodjam") in central BC (Figure 1).  The Woodjam project is home to the large porphyry-related Southeast copper and gold deposit, plus several other porphyry-related deposits and zones.

HIGHLIGHTS

  • Strong DCIP chargeability-high anomaly outlined in the Great Plains target area

  • Area is inferred to be geologically analogous to the nearby Southeast deposit

  • Thin veneer of glacial till may have hidden mineralization from previous operators

"Part of our rationale for acquiring the Woodjam property was the prospectivity away from known mineralization," commented Craig Parry, Executive Chairman. "The Great Plains target area is a perfect example of this. It has the right geology and plenty of room for discoveries with scale."

"These DCIP results are compelling," commented Steve Blower, Vice President of Exploration. "We know that Woodjam porphyry-related mineralization responds well to DCIP surveying, so a large and strong chargeability anomaly in a previously unexplored area inferred to have similar geology as the large Southeast deposit is exciting." 

The DCIP Survey

The 2024 Great Plains reconnaissance DCIP surveying consisted of 17 line-kms across 6 survey lines, extending existing IP coverage2 at Woodjam 3 km to the south (Figure 1). The survey was designed to detect and characterize sulphide mineralization at Great Plains, which is commonly present in porphyry-related mineral systems.

The Great Plains target area is interpreted to be underlain by similar geology as the Southeast deposit, located approximately 4 km to the north. Southeast has a historical inferred mineral resource estimate of 221.7 million tonnes grading 0.31% copper and 0.05 g/t gold1. Mineralization at Southeast is hosted near the western margin of the ~200 million year old, district-scale Takomkane batholith. Based on existing geophysical data, this prospective contact is interpreted to continue along strike across the Woodjam Project to the south for at least nine kilometres.  This broad corridor of prospective geology, known as the Great Plains target area, is essentially unexplored due to a ubiquitous thin veneer of glacial till that conceals the bedrock.

The DCIP survey successfully identified a broad (at least 2km x 2km) chargeability-high anomaly (Figure 2).  The size and intensity of the anomaly is similar to other anomalies associated with known porphyry-related copper and gold systems at Woodjam, including the Southeast deposit.