Drilling hit multiple zones of palladium-dominant mineralization including a footwall copper sulfide vein containing 1.2 ounces per tonne palladium. Drilling results received over the last ten months combined with geophysical data confirm the presence of a persistently mineralized layer along the base of the
Highlights
Drillhole EBL 21-09 intersected three discrete zones of palladium-rich sulfide mineralization including a footwall copper sulfide vein which grades 37.6 g/t Pd (1.2 oz/tonne Pd), 6.68 g/t Pt and 21.3% Cu over 0.54 metres within a two metre mineralized interval averaging 10.7 g/t Pd and 5.87% Cu. Similar grades are present in footwall copper sulfide veins in major magmatic systems, globally - including both the
Drill hole EBL21-07, drilled 70 metres southeast from EBL21-09, also intersected wide zones of palladium mineralization having local higher-grade sections including 1.0 metres of 11.5 g/t Pd from 6.0 metres depth.
EBL21-08, the most northerly and westerly hole drilled in the target area, is a 350 metre step out from the main area of drilling. It intersected a narrow, higher-grade section in the Basal Layer (0.75 metres with 4.64 g/t Pd and 1.19 Pt).
The area between hole EBL21-08 in the west and holes EBL21-07 and 09 in the east is over 200 metres wide and is centered on a potential north-striking feeder fault that remains to be drilled.
Palladium mineralization continues to be associated with an extensive, inclusion-rich gabbro layer that blankets the base of the
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