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Coppermine Geology
- All first-order controls for a sediment-hosted copper deposit – with a proof-of-concept historic drilling result
- Right time, right place: Proterozoic Era basins host some of the largest sediment hosted copper deposits
- Well-endowed district: Evidence of copper-fertile hydrothermal fluids is present throughout the project, evidenced by the numerous volcanic hosted showings
Optionality: High grade volcanic hosted vein and breccia systems with sediment hosted copper potential offers pipeline of drill targets
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Large Scale Copper Potential at the Pre Discovery Stage
- Rae is less than 70km from Kugluktuk, a 24/7 airstrip and Port.
- The district is best known for the ‘Coppermine River Group’ basalts which feature extremely high grade copper showings of >45% Cu
- Rae is visually stunning with its wide spread chalcocite dominant vein systems
- The area came to the attention of European explorers in the 17th Century when tools and idols made of native copper by the local Inuit were observed
- Prospector Samuel Hearne reached the area in 1771 and reported finding a 2 kg copper nugget at surface
- Numerous locations occur throughout the project area where native copper or copper sulphides are found disseminated in sedimentary rocks – native copper was identified during the field trip.
- Modern exploration by Tundra Copper Corp. and Kaizen Discovery Corp between 2013-2015 reconfirmed the high grade volcanic hosted copper using modern lab techniques with several samples > 40% Cu and a 2015 exploration drillhole returned 28.97m at 0.57% Cu within the overlying sedimentary package, confirming the presence of sediment-hosted copper deposits.
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2024 Field Campaign
- Large scale copper discovery confirmed
- Multiple high-grade copper vein systems identified
- Vision – a ±10km long NE/SW structural corridor, feeding from the Herb Dixon regional fault covering the Don and Pat project areas; results include:
- Don: 64.02% Cu & 152 g/t Ag (F005965) 62.02% Cu & 162 g/t Ag (F005966) and 50.48% Cu & 102 g/t Ag (F005959).
- Pat: 55.01% Cu (F005977), 46.07% Cu (F005984), 44.43% Cu (F005979) and 43.10% Cu (F005985)
- Rocket – an area ±400m x 200m containing dominant chalcocite vein systems: 54.12% Cu (F005950), 53.82% Cu (F005949), 53.47% Cu (F005935), 53.24% Cu (F005944) and 51.59% Cu (F005942)
- Thor – host to the historic HALO occurrence, >800mtrs of outcropping mineralization identified: 54.02% Cu (F005921), 25.7% Cu (F005922), 24.4% Cu (F005927) and 24.1% Cu (F005931)
Sedimentary Hosted Copper
- All first-order controls for a sediment-hosted copper deposit – with a proof-of-concept historic drilling result <2km east of our licence boundary
- Right time, right place: Proterozoic Era basins host some of the largest sediment hosted copper deposits
- Well-endowed district: Evidence of copper-fertile hydrothermal fluids is present throughout the project, evidenced by the numerous volcanic hosted showings
- Optionality: High grade volcanic hosted vein and breccia systems with sediment hosted copper potential offers pipeline of drill targets
Hulk – a district scale conductive anomaly
- Three, fault controlled, sub basins covering > 20km of strike across the Rae Group sedimentary structure within the Hulk target area
Hulk – 3 distinct fault bounded sedimentary sub-basins
- Massive Upside – Anomalies open to the north

Inverted conductivity section along line 7740 (N/S), lookingg East through the basalt-sediment contact. A gently north dipping conductive zone over >10km, is observed through the sub basin
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Profile of total magnetic intensity along line 7740 (N/S) through the basalt-sediment contact within Hulk sub basin target
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View from the northwest of the Company’s claims, looking southeast through the Hulk target
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View looking north, slice through the resistivity voxel illustrating the interpreted sub basin architecture at the Hulk exploration district. Voxel is sliced E/W through a northing of 7513500 NAD83 / UTM Zone 11N
Stark – a target in its own right? And – it is feeding Hulk
- Herb Dixon fault: a major, regional N/S fault covering >25km through the Company’s Rae Project that intersects the Hulk area.
- It can be traced to the Vision target where assays from rock chips included results of 64.02%, 62.02%, 55.01% and 50.48% Cu
- The Stark target, situated on the Herb Dixon fault presents a highly conductive signature over more than 14km strike length and up to 2.2km wide that is coincident within a well-defined structure
Danvers – An opportunity to accelerate the pathway to an initial resource for the Rae area
- The historic non JORC resource estimate of 4.16mt @ 2.96% Cu represents the most significant deposit discovered within the broader Coppermine area
- Historical drilling highlights include:
- o47.10m @ 3.23 % Cu from 42.2m (S-24)
- o39.40m @ 4.91 % Cu from 60.3m (S-57)
- o35.40m @ 3.18 % Cu from 21.0m (S21)
- o31.4m @ 3.26 % Cu from 15.2m (S-20)
- o27.5m @ 4.09 % Cu from 76.7m (S-63)
- Recent drilling confirmed the resource is open in all directions:
- o98.05m @ 0.93 % Cu from 65.86m (2003-47-3)
- o72.70m @ 1.63 % Cu from 26.46m (2003-47-2)
- o56.39m @ 1.48% Cu from 47.00m (2003-47-1)
- o52.88m @ 1.16 % Cu from 176.99m (2005-47-7)
- o61.24m @ 0.69 % Cu from 142.08m (2005-47-8)