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Blende Silver Engages Ronacher McKenzie Geoscience to Advance District-Scale Interpretation and Targeting Following Promising 3D IP Survey Results at Flagship Yukon Project
April 27, 2026 – TheNewswire - Vancouver, Canada – Blende Silver Corp. (the “Company”) (TSX.V: BAG) (OTC: BAGGF) (WKN: A2QKT9) (FSE: BCW1) is pleased to
About this update from Blende Silver Corp.
[{"type":"text","content":"April 27, 2026 – TheNewswire - Vancouver, Canada – Blende Silver Corp. (the “Company”) (TSX.V: BAG) (OTC: BAGGF) (WKN: A2QKT9) (FSE: BCW1) is pleased to announce that it has engaged Ronacher McKenzie Geoscience Inc. (“RMG”), a leading Canadian geoscience consulting firm, to complete an integrated geological, geochemical, and geophysical interpretation and targeting program at its 100%-owned Blende Silver-Zinc-Lead Project in north-central Yukon. The engagement is driven by compelling initial results from an in-house desktop review of a 3D induced polarization (IP) survey completed over a portion of the project. The survey was designed to calibrate the geophysical signature over the known West Zone mineralization (the anchor of the Company’s existing mineral resource) and to test for potential extensions and new targets across a broader portion of the property, including the ~2 km “Central Zone” gap between the West Zone and East Zone deposits, as well as areas to the north of the West and Central Zones. Key observations from the initial plot-up and inversion of the 3D IP data include: Strong correlation between the IP chargeability response over the West Zone and the known silver-zinc-lead mineralization, providing a reliable calibration benchmark for the property. Identification of multiple significantly larger-scale untested chargeability anomalies, notably in the Lower Central Zone and New Mountain Top areas. These anomalies appear to be several times larger than the chargeability response associated with the defined West Zone mineralization. The Lower Central Zone anomaly and the New Mountain Top anomaly both extend to the edges of the surveyed grid, suggesting potential for greater extent beyond current coverage. Historical drilling in the Central Zone (13 holes drilled along and down the spine of the ridge toward the East Zone) appears, based on the initial inversion data review, to have been positioned between two distinct chargeability anomalies (the Lower Central and Backside Central Zone anomalies) rather than directly testing the strongest responses. These findings suggest the potential for greater system scale and continuity than previously recognized, including possible extensions of mineralization from the West Zone through the Central Zone area toward the East Zone, as well as additional mi...