Highlights
- Nine of first twelve holes with intervals of greater than 1% nickel
- First twelve holes confirm high grade mineralization over 400 metres of strike length that remains open to the north and at depth
- High grade intervals within thick mineralized sections include:
- Hole 22-03: 5.2 metres of 2.60% nickel within 21.0 metres of 1.22% nickel within 91.5 metres of 0.50% nickel from 58.5 metres
- Hole 22-06: 4.0 metres of 2.43% nickel within 12.0 metres of 1.45% nickel within 28.0 metres of 0.77% nickel from 76.5 metres
The Company has drilled a total of 39 holes and 9,670 metres, completing its initial phase to support the development of a mineral resource at Texmont expected to be delivered later this year.
Figure 1: Plan View of Texmont – Historic Drill results Overlain on TMI
Figure 2: Texmont Property – Southern Portion
Mark Selby, Chair & CEO of Canada Nickel Company, said,
Texmont Nickel Property
The Texmont Property is located 36 kilometres south of Timmins. It is considered to be a komatiite flow rather than a dunite sill with sections of highly mineralized peridotite and dimensions approximately 1.2 kilometres long by up to 150 metres wide (see Figure 1).
Canada Nickel has drilled 39 drill holes to date, 34 of which targeted the known mineralization and five of which targeted a possible north extension (Figure 2). This news release contains the assay results from the first 12 holes totaling 3,204 metres (see Tables 1,2). Historic drilling confirms the mineralization pinches out to the south but remains open to the north and at depth. Further drilling to the north of the former mine shaft intersected thick sections of mineralized peridotite but assay results are not yet available. This drilling is expected to be incorporated, along with historic drilling by Fletcher Nickel (which drilled 28,883 metres from 2006-2008) into an initial resource estimate to be released later this year.
Table 1: Texmont exploration drilling results high grade highlights
| Hole ID | From | To | Length* | Ni | Co | Pd | Pt | S |
| (m) | (m) | (m) | ( %) | ( %) | (g/t) | (g/t) | ( %) | |
| TEX22-01 | 22.0 | 44.1 | 22.1 | 0.52 | 0.01 | 0.042 | 0.036 | 0.34 |
| TEX22-02 | 10.5 | 56.2 | 45.7 | 0.55 | 0.02 | 0.041 | 0.033 | 0.45 |
| Including | 27.0 | 33.0 | 6.0 | 1.08 | 0.03 | 0.094 | 0.079 | 0.66 |
| TEX22-03 | 58.5 | 150.0 | 91.5 | 0.50 | 0.01 | 0.031 | 0.023 | 0.45 |
| Including | 129.0 | 150.0 | 21.0 | 1.22 | 0.03 | 0.108 | 0.070 | 1.09 |
| Including | 138.8 | 144.0 | 5.2 | 2.60 | 0.06 | 0.265 | 0.226 | 2.46 |
| And | 131.0 | 132.0 | 0.5 | 6.85 | 0.16 | 0.513 | 0.055 | 5.97 |
| TEX22-04 | 127.3 | 161.5 | 34.2 | 0.56 | 0.02 | 0.046 | 0.046 | 0.33 |
| Including | 145.5 | 151.0 | 4.4 | 0.99 | 0.03 | 0.073 | 0.056 | 0.61 |
| TEX22-05 | 201.0 | 226.0 | 25.0 | 0.48 | 0.02 | 0.036 | 0.028 | 0.54 |
| including | 219.0 | 226.0 | 7.0 | 0.74 | 0.02 | 0.063 | 0.048 | 0.85 |
| TEX22-06 | 76.5 | 105 | 28.5 | 0.77 | 0.02 | 0.065 | 0.071 | 0.91 |
| including | 82.5 | 94.5 | 12.0 | 1.45 | 0.04 | 0.137 | 0.156 | 1.74 |
| including | 88.0 | 92.0 | 4.0 | 2.43 | 0.06 | 0.246 | 0.314 | 2.94 |
| including | 90.1 | 90.6 | 0.5 | 10.6 | 0.25 | 1.200 | 1.680 | 12.4 |
| TEX22-07 | 106.5 | 132.0 | 25.5 | 0.50 | 0.02 | 0.030 | 0.024 | 0.61 |
| including | 106.5 | 114.0 | 7.5 | 0.79 | 0.02 | 0.068 | 0.046 | 0.97 |
| TEX22-08 | 70.7 | 84.0 | 13.3 | 0.51 | 0.02 | 0.033 | 0.024 | 0.48 |
| including | 70.7 | 74.0 | 3.3 | 1.12 | 0.03 | 0.097 | 0.065 | 1.13 |
| TEX22-11 | 93.0 | 139.5 | 46.5 | 0.57 | 0.02 | 0.036 | 0.033 | 0.67 |
| including | 94.5 | 109.5 | 15.0 | 1.06 | 0.03 | 0.081 | 0.073 | 1.32 |
| * True widths are unknown |
Table 2: Texmont exploration drilling results – downhole average
| Hole ID | From | To | Length* | Ni | Co | Pd | Pt | Cr | Fe | S |
| (m) | (m) | (m) | ( %) | ( %) | (g/t) | (g/t) | ( %) | ( %) | ( %) | |
| TEX22-01 | 8.3 | 249.0 | 240.7 | 0.29 | 0.01 | 0.015 | 0.014 | 0.17 | 6.01 | 0.44 |
| TEX22-02 | 6.0 | 126.0 | 120.0 | 0.34 | 0.01 | 0.021 | 0.019 | 0.12 | 5.35 | 0.47 |
| TEX22-03 | 1.8 | 150.0 | 148.2 | 0.40 | 0.01 | 0.021 | 0.017 | 0.14 | 5.26 | 0.39 |
| TEX22-04 | 127.3 | 307.5 | 200.2 | 0.31 | 0.01 | 0.019 | 0.017 | 0.15 | 5.72 | 0.33 |
| TEX22-05 | 39.0 | 401.8 | 362.8 | 0.18 | 0.01 | 0.010 | 0.010 | 0.14 | 6.75 | 0.25 |
| Including | 189.7 | 345.5 | 155.8 | 0.28 | 0.01 | 0.014 | 0.012 | 0.13 | 5.51 | 0.31 |
| TEX22-06 | 14.2 | 300.0 | 285.8 | 0.24 | 0.01 | 0.013 | 0.014 | 0.11 | 5.97 | 0.37 |
| TEX22-07 | 6.0 | 300.0 | 294.0 | 0.24 | 0.01 | 0.011 | 0.011 | 0.16 | 6.32 | 0.45 |
| and | 199.8 | 300.0 | 100.2 | 0.33 | 0.01 | 0.010 | 0.009 | 0.15 | 5.31 | 0.47 |
| TEX22-08 | 9.3 | 282.0 | 272.7 | 0.22 | 0.01 | 0.008 | 0.008 | 0.15 | 5.77 | 0.28 |
| Including | 61.5 | 163.5 | 102.0 | 0.31 | 0.01 | 0.010 | 0.009 | 0.15 | 5.27 | 0.33 |
| TEX22-09 | 9.0 | 252.0 | 243.0 | 0.20 | 0.01 | 0.010 | 0.010 | 0.14 | 6.68 | 0.34 |
| Including | 110.0 | 159.3 | 49.3 | 0.35 | 0.01 | 0.017 | 0.013 | 0.14 | 5.84 | 0.49 |
| and | 180.0 | 244.5 | 64.5 | 0.28 | 0.01 | 0.008 | 0.008 | 0.18 | 5.60 | 0.39 |
| TEX22-10 | 7.5 | 255.0 | 247.5 | 0.18 | 0.01 | 0.007 | 0.007 | 0.16 | 6.19 | 0.66 |
| Including | 86.5 | 151.7 | 65.2 | 0.25 | 0.01 | 0.006 | 0.006 | 0.16 | 5.20 | 0.22 |
| TEX22-11 | 6.6 | 222.8 | 216.2 | 0.28 | 0.01 | 0.013 | 0.014 | 0.18 | 6.37 | 0.41 |
| including | 93.0 | 222.8 | 129.8 | 0.37 | 0.01 | 0.017 | 0.017 | 0.16 | 5.90 | 0.44 |
| and | 236.1 | 303.0 | 66.9 | 0.25 | 0.01 | 0.008 | 0.009 | 0.15 | 5.51 | 0.28 |
| TEX22-12 | 62.0 | 141.6 | 79.6 | 0.23 | 0.01 | 0.007 | 0.007 | 0.15 | 5.27 | 0.21 |
| and | 164.0 | 211.0 | 47.0 | 0.21 | 0.01 | 0.006 | 0.005 | 0.18 | 6.12 | 0.37 |
TEX22-01 was collared directly over komatiite, and intersected a thick sequence of mineralized peridotite, ending in strongly serpentinized dunite, with minor dykes encountered near the top of the hole. The hole averaged 0.29% Ni over 240.7 metres, including a higher-grade section of 0.52% Ni over 22.1 metres (see Table 3 for all high grade composites, and Table 4 for whole mineralized lengths).
TEX22-02 was collared 100 metres northeast of TEX22-01 and intersected mineralized komatiite 6 metres below surface, intersecting mineralized peridotite for a length of 120.0 metres until encountering gabbro at the lower contact. The hole averaged 0.34% nickel over 120.0 metres, including 0.55% nickel over 45.7 metres from 10.5 metres downhole.
TEX22-03 was collared with an east azimuth 20 metres southwest of the existing mining shaft and intersected mineralized peridotite from 1.8 meters to the end of hole at 150.0 metres. The hole averaged 0.40% nickel over 148.2 metres, including 1.22% nickel and 0.18 g/t Pt+Pd over 21.0 metres.
TEX22-04 was collared within the hanging wall intersecting mafic volcanics and then gabbro before encountering mineralized peridotite. The mineralized peridotite averaged 0.31% Ni over 200.2 metres, including 0.56% Ni over 34.2 metres. The hole intersected the footwall, ending in mafic volcanics and giving a good indication of the overall thickness of the mineralized ultramafics.
TEX22-05 was collared in hanging wall mafic volcanics and was aimed to cut across the strike length of the mineralized komatiite. The hole intersected 362.8 metres of peridotite averaging 0.18% Ni over 362.8 metres, including 42.0 metres of 0.41% nickel. A few minor dykes were encountered within the hole.
TEX22-06 was drilled 100 m southeast of TEX22-03 in komatiite and intersected mineralized peridotite, with minor intersections of late dykes. The hole averaged 0.24% nickel over 285.8 metres, including a high-grade section of 1.45% nickel and 0.28 g/t Pt+Pd over 12.0 metres.
TEX22-07 was collared 100 southeast of TEX22-03, intersecting komatiite followed by a moderate to strongly mineralized peridotite, interrupted by minor diabase dykes. The hole averaged 0.24% Ni over 294.0 metres including 0.33% Ni over 100.2 metres and 0.41% Ni over 43.5 metres.
TEX22-08 was collared 50 metres south of TEX22-07 and drilled to the west. The hole started in komatiite and continued into peridotite, ending in peridotite. The hole averaged 0.22% Ni over 272.7 metres including 0.31% Ni over 100.2 metres.
TEX22-09 was collared at the same location as TEX22-08 but at a steeper dip (-70o versus -50o). The hole started in komatiite and continued into peridotite, ending in peridotite. Mineralization averaged 0.20% Ni over 243.0 metres, including 0.28% Ni over 64.5 metres and 0.35% Ni over 49.3 metres.
TEX22-10 was collared 50 metres south of TEX22-08 and intersected a thick section of mineralized peridotite interrupted by a minor sliver of metasedimentary rocks. The hole averaged 0.18% Ni over 247.5 metres including 0.24% over 75.0 metres.
TEX22-11 was collared at the same location as TEX22-10 but drilled at a steeper angle. The hole intersected two sections of mineralized peridotite, 0.28% Ni over 216.2 metres and 66.9 metres of 0.25% Ni, with the intervals separated by metasedimentary rocks. The upper mineralized interval included a higher-grade section of 129.8 metres of 0.37% and 19.5 metres of 0.96% Ni.
TEX22-12 was collared 50 metres south of TEX22-10 and intersected 2 sections of mineralized peridotite separated by metasediments, the upper section averaging 0.23% Ni over 79.5 metres, and the lower section averaging 0.21% Ni over 47.0 metres.
About Canada Nickel Company
Canada Nickel Company Inc. is advancing the next generation of nickel-sulphide projects to deliver nickel required to feed the high growth electric vehicle and stainless-steel markets. Canada Nickel Company has applied in multiple jurisdictions to trademark the terms NetZero NickelTM, NetZero CobaltTM, NetZero IronTM and is pursuing the development of processes to allow the production of net zero carbon nickel, cobalt, and iron products. Canada Nickel provides investors with leverage to nickel in low political risk jurisdictions. Canada Nickel is currently anchored by its 100% owned flagship Crawford Nickel-Cobalt Sulphide Project in the heart of the prolific Timmins-Cochrane mining camp. For more information, please visit www.canadanickel.com