$PNPNF announce the discovery of a new high-grade Cu-PGE mineralized zone approximately 5km northeast of the main Nisk deposit. The target area was never previously drilled and was identified as "Wildcat." It is characterized by a strong magnetic anomaly from an ultramafic unit previously mapped in the surface outcrop. Ultramafic rocks consistent with the main Nisk deposit were intersected in hole PN-23-031A, but the high-grade mineralization is hosted in amphibolite and tonalite, which lie on top of the ultramafic sequence.
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