Drillhole GL26029 intersected semi-massive to massive pyrrhotite-pentlandite-chalcopyrite veins and breccias across 21.44 m of mineralized drill core to the southwest of the Gochager Lake Ni-Cu-Co Deposit, returning >1% Ni across zones of increased sulphide abundance.
The mineralized intercept is approximately 75 m outside of the maiden MRE, approximately 150 m west of high-grade mineralization inside the MRE open pit shell and remains open to the southwest. There is strong potential to expand the maiden MRE to include this mineralized intercept in GL26029….
Beyond the Headline
Following its release of a maiden MRE, Fathom Nickel reported that Hole GL26029, located 75m south southwest of the MRE, intersected 21.44 m @ 0.24% Ni from 199.13m, containing 6.78 m @ 0.42% Ni and several additional narrow semi-massive/massive sulphide intervals exceeding 1% Ni.
Northeast of the MRE, GL26028 and GL26030 intersected a new sulphide zone approximately 155 m outside the MRE. GL26030 returned 54.79 m of mineralized core, albeit at only 0.12% Ni overall. This hole also returned a 1.99 g/t Pt over 0.31m confirming PGE mineralization in the system.
As noted for the September 10, 2026 release, the MRE pit only covers a small portion of the approximately 8km prospective trend. These drill results show the potential to further expand the maiden resource as well as discover additional Ni-Cu deposits on this important trend.