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Kingfisher Identifies New Porphyry Copper System Below Hank Gold-Silver Deposits at Hwy 37 Project, Golden Triangle
VANCOUVER, BC / ACCESS Newswire / September 23, 2025 / Kingfisher Metals Corp. (TSXV:KFR)(FSE:...
About this update from Kingfisher Metals Corp
[{"type":"text","content":"Kingfisher Identifies New Porphyry Copper System Below Hank Gold-Silver Deposits at Hwy 37 Project, Golden TriangleVANCOUVER, BC / ACCESS Newswire / September 23, 2025 / Kingfisher Metals Corp. (TSXV:KFR)(FSE:970)(OTCQB:KGFMF) (\"Kingfisher\" or the \"Company\") is pleased to announce the identification of a new porphyry copper system below the Hank epithermal gold-silver system at the HWY-37 project. Additionally, the program at HWY 37 is complete for the 2025 exploration program and crews have been demobilized from site. The 849 km2 HWY 37 Project is located within the Golden Triangle, British Columbia.HW-25-011 Highlights:Identification of a new porphyry copper system below the Hank epithermal gold - silver deposits.The redrill of the Lower Hank Porphyry target (HW-25-011) intercepted a new porphyry copper system over 429 meters (m). This intercept is significant as it demonstrates the potential for a large porphyry copper-gold system nested below the broad Hank epithermal gold-silver system (Figures 1-3).The gold-silver mineralization observed at surface at Hank is considered to be related to the alteration and mineralization observed in HW-25-011.Alteration and mineralization observed in HW-25-011 is interpreted to be in a proximal position, on the margins of a conceptual porphyry core.Figure 1: Hank Porphyry Target Plan View Summary of HW-25-011 & The Hank Porphyry TargetThe planned depth of HW-25-011 was 650 m, however, it was extended to a final depth of 959 m based on observations of the drill core and to collect targeting data for follow-up drilling in 2026. Porphyry style alteration and mineralization was first observed at 530 m downhole depth and continued over 429 m with the end of hole (959 m) bottoming in copper mineralization.Additional induced polarization (IP) geophysical survey data collected in 2025 helped to further refine the compelling geophysical signature of this target. High chargeability domains (30-70 mV/V) flank a broad domain of moderate to high chargeability (20-30 mV/V) in this area (Figure 2). This is interpreted to represent a pyrite-dominant shell lateral to a copper-sulfide dominant core. IP resistivity also shows a broad resistive feature that is interpreted to represent a resistive porphyry intrusive core surrounded by conductive clay alteration (Figure 3). Airborne magnetics show a broa...