Highlights
- Acquisition of 13 additional target properties consolidates district scale potential.
- Combined target surface footprint of 37.7 square km – 40 times larger than current
Crawford Main Zone resource of 0.85 square km. - Ten target properties have larger footprint than Crawford and nine confirmed to contain the same host mineralization as Crawford.
- Sothman target property has historical higher grade, shallow resource of approximately 190,000 tons of 1.24% nickel (with 300 metres strike length)1; remaining 2.2 km of strike length is largely untested.
- Four target areas have yielded drill intersections of > 0.3% nickel including:
- Sothman: 2.31% nickel and 0.19% copper over true width of 3.2 metres within 1.58% nickel and 0.12% copper over true width of 8.6 metres from 41 metres;
Deloro : 0.38% nickel and 0.22 g/t PGM over core length of 15.5 metres within 0.28% nickel and 0.09 g/t PGM over core length of 299 metres from 241 metres;- Midlothian: 0.24% nickel over core length of 345 metres, including 0.30% nickel over 42 metres;
- Mann Southeast: multiple 3 metre intervals grading 0.31-0.33% nickel within 111 metres of dunite across entire core length
"The acquisition of these highly prospective target properties represents a transformational milestone for
______________________ |
1 See Statement Regarding Historical Resource Estimates on page 27 of this press release. |
2 See Preliminary Economic Assessment, titled "Crawford Nickel-Sulphide Project National Instrument 43-101 Technical Report and Preliminary Economic Assessment", with an effective date of |
Figure A –
The Company will host a conference call and webcast today,
Sothman
Sothman is a property of approximately 1,000 ha located 70 km south of Timmins. The project was acquired from Glencore.
The Sothman Property contains an ultramafic sill comprised mainly of dunite (see Figure 2) that is estimated to be up to 200-300 metres thick, 2.2 km long and open at depth. An unclassified historical resource estimate reported as 189,753 tons grading 1.24% nickel (the
Drillhole DG53-S41A is the only hole drilled in the eastern area of the
Table 1a – Historical Drilling –
Hole ID | From (m) | To (m) | Length (m) | Estimated True | Ni % | Cu % |
SM56-K11 | 93.2 | 102.4 | 9.2 | 4.6 | 1.58 | 0.17 |
including | 93.2 | 97.5 | 4.3 | 2.2 | 2.58 | 0.34 |
SM67-B06 | 28.7 | 40.5 | 11.8 | 8.4 | 1.57 | 0.11 |
including | 28.7 | 33.8 | 5.1 | 3.6 | 2.28 | 0.16 |
DG50-S04 | 41.2 | 53.3 | 12.2 | 8.6 | 1.58 | 0.12 |
including | 41.2 | 45.7 | 4.6 | 3.2 | 2.31 | 0.19 |
DG51-S20 | 89.9 | 95.8 | 5.9 | 4.0 | 1.56 | 0.13 |
DG50-S05 | 19.8 | 21.0 | 1.2 | 0.9 | 7.51 | 0.62 |
SM71-1 | 398.1 | 409.0 | 11.0 | 4.1 | 0.66 | 0.04 |
___________________________ |
3 See Statement Regarding Historical Resource Estimates on page 27 of this press release. |
Table 1a – Historical Drilling –
Hole ID | From (m) | To (m) | Length (m) | Estimated True | Ni % | Cu % |
including | 398.1 | 401.4 | 3.4 | 1.2 | 1.32 | 0.05 |
SM71-2 | 353.3 | 358.8 | 5.5 | 2.5 | 0.49 | 0.03 |
Table 1b – Historical Drilling – Sothman Property – Selected Lithologies
Hole ID | From (m) | To (m)* | Rock Type |
DG-50-S04 | 32.4 | 107.9 | Ultramafics - Peridotite |
DG-50-S05 | 22.9 | 82.0 | Ultramafics - Peridotite |
DG-51-S09 | 7.3 | 217.0 | Ultramafics - Peridotite |
DG-51-S12 | 7.0 | 111.4 | Ultramafics - Peridotite |
DG-51-S12 | 111.4 | 114.1 | Ultramafics - Gabbro |
DG-51-S12 | 114.1 | 118.3 | Ultramafics - Peridotite |
DG-51-S12 | 118.3 | 142.8 | Ultramafics - Gabbro |
DG-51-S20 | 19.8 | 96.9 | Ultramafics - Peridotite |
DG-53-S41A | 23.8 | 83.8 | Ultramafics - Peridotite |
SM-56-K11 | 85.7 | 148.4 | Ultramafics - Peridotite |
SM-67-B06 | 25.5 | 101.8 | Ultramafics - Peridotite |
SM-67-B25 | 36.6 | 91.1 | Ultramafics - Peridotite |
SM-67-B26 | 7.6 | 120.1 | Ultramafics - Peridotite |
SM-67-B27 | 12.2 | 121.6 | Ultramafics - Peridotite |
SM-67-B28 | 15.2 | 47.7 | Ultramafics - Peridotite |
SM-71-01 | 394.0 | 426.7 | Ultramafics - Peridotite |
SM-71-02 | 351.1 | 366.7 | Ultramafics - Peridotite |
* Denotes ended in mineralization |
Figure 1 – Sothman Property – Historical Drillholes Over Total Magnetic Intensity ("TMI").
All five holes noted presence of magnetite (up to 20-25% magnetite in interval 39.4-89.5 metres from hole FY-02-02) and disseminated sulphides. Only specific non-consecutive intervals were assayed. Two of the four holes had nickel mineralization exceeding 0.40% nickel: FY02-02 with 0.42% nickel over a core length of 4.2 metres, with up to 0.73 g/t Pd and 0.23 g/t Pt over 1.2 metres, and FY-02-10 with 0.48% nickel, 0.28 g/t Pd, and 0.14 g/t Pt over 2.8 metres. See Table 2a and 2b below.
Figure 2 – Deloro Property – Historical Drillholes Over TMI
Table 2a – Historical Drilling – Deloro Property – Significant Intersections*
Hole ID | From (m) | To (m) | Length (m) | Ni % | Cu % | Pd g/t | Pt g/t |
FY-02-02 | 241.0 | 314.5 | 73.5 | 0.28 | 0.03 | 0.06 | 0.03 |
Including | 299.0 | 314.5 | 15.5 | 0.38 | 0.06 | 0.15 | 0.07 |
FY-02-02 | 324.2 | 345.0 | 20.8 | 0.24 | 0.03 | 0.03 | 0.01 |
including | 342.8 | 343.1 | 0.4 | 0.74 | 0.23 | 0.16 | 0.17 |
FY-02-10 | 54.7 | 59.7 | 5.0 | 0.27 | 0.03 | 0.01 | 0.00 |
FY-02-10 | 95.8 | 98.6 | 2.8 | 0.48 | 0.03 | 0.28 | 0.14 |
FY-02-13 | 122.8 | 152.9 | 30.1 | 0.25 | 0.01 | 0.02 | 0.01 |
FY-02-13 | 177.5 | 200.5 | 23.0 | 0.24 | <0.01 | 0.00 | 0.00 |
FY-02-13 | 298.0 | 318.0 | 20.0 | 0.26 | <0.01 | 0.00 | 0.00 |
* Insufficient drilling completed to determine dip and true width of orebody |
Table 2b – Historical Drilling – Deloro Property – Selected Lithologies
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
FY-02-01 | 4.0 | 11.0 | 7.0 | Peridotite |
FY-02-01 | 11.0 | 14.1 | 3.1 | Serpentinite |
FY-02-01 | 14.8 | 18.2 | 3.4 | Serpentinite |
FY-02-01 | 18.2 | 29.9 | 11.7 | Peridotite |
FY-02-01 | 29.9 | 31.3 | 1.4 | Peridotite |
FY-02-01 | 31.3 | 34.8 | 3.5 | Peridotite |
FY-02-01 | 36.5 | 98.5 | 62.0 | Peridotite |
FY-02-01 | 98.5 | 102.0 | 3.5 | Serpentinite |
FY-02-02 | 5.8 | 21.3 | 15.5 | Peridotite/Dunite |
FY-02-02 | 23.1 | 33.7 | 10.6 | Peridotite/Dunite |
FY-02-02 | 33.7 | 34.7 | 1.0 | Serpentinite |
FY-02-02 | 39.4 | 89.5 | 50.1 | Peridotite/Dunite |
FY-02-02 | 89.5 | 90.4 | 0.8 | Pyroxenite |
FY-02-02 | 92.1 | 117.1 | 25.0 | Peridotite/Dunite |
FY-02-02 | 117.1 | 120.7 | 3.6 | Serpentinite |
FY-02-02 | 132.5 | 134.4 | 1.9 | Peridotite |
FY-02-02 | 135.4 | 136.8 | 1.4 | Pyroxenite |
FY-02-02 | 137.1 | 138.6 | 1.5 | Serpentinite |
FY-02-02 | 138.6 | 149.8 | 11.2 | Peridotite/Dunite |
FY-02-02 | 151.7 | 206.1 | 54.4 | Peridotite/Dunite |
FY-02-02 | 210.6 | 217.9 | 7.2 | Serpentinite |
FY-02-02 | 219.3 | 314.7 | 95.4 | Peridotite |
FY-02-02 | 316.7 | 319.0 | 2.3 | Pyroxenite |
FY-02-02 | 319.0 | 319.7 | 0.7 | Peridotite |
FY-02-02 | 319.7 | 321.2 | 1.5 | Peridotite/Dunite |
FY-02-02 | 321.2 | 324.2 | 3.0 | Peridotite |
FY-02-02 | 324.2 | 324.8 | 0.6 | Peridotite |
FY-02-02 | 324.8 | 325.8 | 1.0 | Peridotite |
FY-02-02 | 325.8 | 332.2 | 6.4 | Peridotite |
FY-02-02 | 332.2 | 333.5 | 1.3 | Serpentinite |
FY-02-02 | 333.5 | 339.7 | 6.2 | Peridotite |
FY-02-02 | 339.7 | 365.7 | 26.0 | Serpentinite |
FY-02-02 | 373.5 | 381.1 | 7.7 | Serpentinite |
FY-02-06 | 25.0 | 110.3 | 85.3 | Serpentinite |
FY-02-06 | 110.9 | 208.9 | 98.0 | Serpentinite |
Table 2b – Historical Drilling – Deloro Property – Selected Lithologies (continued)
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
FY-02-06 | 211.2 | 301.0 | 89.8 | Serpentinite |
FY-02-10 | 31.7 | 50.0 | 18.3 | Pyroxenite |
FY-02-10 | 54.7 | 59.7 | 5.0 | Pyroxenite |
FY-02-10 | 69.9 | 73.8 | 3.8 | Peridotite |
FY-02-10 | 75.5 | 97.6 | 22.1 | Pyroxenite/Peridotite |
FY-02-10 | 97.6 | 113.5 | 15.9 | Peridotite/Dunite |
FY-02-10 | 113.5 | 121.9 | 8.4 | Peridotite |
FY-02-10 | 121.9 | 123.5 | 1.7 | Serpentinite |
FY-02-10 | 123.9 | 124.6 | 0.7 | Serpentinite |
FY-02-10 | 124.8 | 130.7 | 5.9 | Peridotite |
FY-02-10 | 130.7 | 135.0 | 4.3 | Peridotite |
FY-02-12 | 52.4 | 58.6 | 6.2 | Pyroxenite |
FY-02-12 | 58.6 | 64.7 | 6.1 | Serpentinite |
FY-02-12 | 75.3 | 79.1 | 3.8 | Serpentinite |
FY-02-12 | 80.0 | 80.3 | 0.3 | Serpentinite |
FY-02-12 | 80.3 | 82.3 | 2.0 | Serpentinite |
FY-02-12 | 85.6 | 86.2 | 0.6 | Serpentinite |
FY-02-12 | 86.2 | 97.3 | 11.1 | Peridotite |
FY-02-12 | 97.3 | 113.5 | 16.2 | Pyroxenite |
FY-02-12 | 113.5 | 118.2 | 4.7 | Peridotite |
FY-02-12 | 119.4 | 122.0 | 2.5 | Peridotite |
FY-02-12 | 122.0 | 133.3 | 11.3 | Peridotite/Dunite |
FY-02-12 | 133.3 | 146.4 | 13.2 | Dunite |
FY-02-12 | 146.6 | 272.0 | 125.4 | Dunite |
FY-02-13 | 114.3 | 156.0 | 41.6 | Peridotite |
FY-02-13 | 166.1 | 168.1 | 2.0 | Peridotite |
FY-02-13 | 168.1 | 171.9 | 3.8 | Peridotite |
FY-02-13 | 171.9 | 177.5 | 5.6 | Dunite |
FY-02-13 | 177.5 | 179.6 | 2.1 | Peridotite |
FY-02-13 | 179.6 | 318.0 | 138.4 | Dunite |
Mann
Mann is located 25 km east of Crawford and totals 7,800 ha. The ultramafic is estimated to be a combined 21 km in length with variable thickness and having at least three main dunitic cores like that at Crawford (Mann Central, Mann Northwest, and Mann Southeast). The Company has acquired the right to earn an 80% interest in the Mann Property from Noble by an initial payment of
Mann Central
The Mann Central Property area covers a single 4 km long by up to 1 km wide ultramafic intrusion (see Figure 3) that is evident in TMI geophysical surveys. Historical drilling has already delineated ultramafic mineralization over a strike length of 2,700 metres and 690 metres wide. Only one historical hole had assays –
Table 3a – Historical Drilling – Mann Central Property – Selected Lithologies
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
INCO-1 | 5.2 | 162.5 | 157.3 | Peridotite |
M-1 | 1.5 | 213.7 | 212.1 | Peridotite |
M-2 | 7.3 | 214.9 | 207.6 | Peridotite |
M-3 | 7.6 | 14.9 | 7.3 | Peridotite |
M-3 | 18.0 | 96.3 | 78.3 | Peridotite |
M-3 | 96.3 | 141.7 | 45.4 | Pyroxenite |
M-3 | 141.7 | 155.1 | 13.4 | Peridotite |
M-3 | 165.8 | 172.8 | 7.0 | Pyroxenite |
M-4 | 11.3 | 50.0 | 38.7 | Dunite |
M-4 | 50.0 | 54.6 | 4.6 | Pyroxenite |
M-4 | 54.6 | 88.4 | 33.8 | Dunite |
M-4 | 88.4 | 191.4 | 103.0 | Peridotite |
M-4 | 191.4 | 196.0 | 4.6 | Pyroxenite |
M-5 | 10.1 | 41.1 | 31.1 | Pyroxenite |
M-5 | 41.1 | 153.3 | 112.2 | Peridotite |
M-5 | 161.5 | 172.5 | 11.0 | Pyroxenite |
M-6 | 7.9 | 114.9 | 107.0 | Peridotite |
M-6 | 123.1 | 128.0 | 4.9 | Pyroxenite |
M-7 | 11.3 | 107.3 | 96.0 | Peridotite |
M-7 | 113.4 | 127.1 | 13.7 | Peridotite |
M-7 | 129.2 | 172.8 | 43.6 | Peridotite |
1A | 0.9 | 7.0 | 6.1 | Peridotite |
1A | 51.5 | 54.6 | 3.1 | Peridotite |
2A | 2.4 | 8.7 | 6.3 | Peridotite |
2A | 22.0 | 52.1 | 30.2 | Peridotite |
2A | 83.8 | 111.3 | 27.4 | Peridotite |
3A | 1.2 | 57.3 | 56.1 | Peridotite |
Table 3a – Historical Drilling – Mann Central Property – Selected Lithologies (continued)
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
3A | 61.3 | 80.5 | 19.2 | Peridotite |
4A | 0.6 | 10.4 | 9.8 | Peridotite |
4A | 11.0 | 37.5 | 26.5 | Peridotite |
MA4-2-76 | 84.4 | 90.8 | 6.5 | Gabbro |
MA4-2-76 | 90.8 | 121.9 | 31.1 | Pyroxenite |
MA4-2-76 | 121.9 | 123.1 | 1.2 | Peridotite |
MA5-1-76 | 102.4 | 108.8 | 6.4 | Gabbro |
MA5-1-76 | 108.8 | 138.1 | 29.3 | Peridotite |
MA5-2-76 | 8.7 | 123.1 | 114.4 | Ultramafic |
MN87-3 | 32.3 | 200.0 | 167.7 | Ultramafic |
MAN43-01 | 9.0 | 188.0 | 179.0 | Ultramafic |
MAN43-03 | 78.6 | 158.0 | 79.4 | Ultramafic |
Table 3b – Historical Drilling – Mann Central Property – Significant Intersections
Hole ID | From (m) | To (m) | Length (m) | Ni % |
MAN43-03 | 89.1 | 90.3 | 1.2 | 0.29 |
MAN43-03 | 95.1 | 95.5 | 0.4 | 0.15 |
MAN43-03 | 107.2 | 107.6 | 0.4 | 0.16 |
MAN43-03 | 116.0 | 116.5 | 0.5 | 0.19 |
MAN43-03 | 122.0 | 122.4 | 0.4 | 0.21 |
MAN43-03 | 131.0 | 131.6 | 0.6 | 0.23 |
MAN43-03 | 142.7 | 143.0 | 0.3 | 0.21 |
MAN43-03 | 149.0 | 149.5 | 0.5 | 0.22 |
Figure 3 – Mann Central Property – Historical Drillholes Over TMI.
Mann Northwest
The Mann Northwest Property covers an ultramafic intrusion having dimensions of 3.5 km long by 600-800 metres wide (see Figure 4). The intrusion is described as mostly peridotite, commonly serpentinized, with overlying leuco-gabbro and pyroxenite.
First Point Minerals Corp. conducted a three-hole drill program (468 metres) in 2002 targeting PGMs in pyroxenites that overlie the ultramafic units. While the first hole (FHR-01-01) targeted the contact between the volcanics and the ultramafic rocks, the second hole (FHR02-02) intersected serpentinized peridotite containing magnetite and some sulphide stringers in fractures. Nickel assays were taken at selected intervals and ranged from a low of 0.10% nickel to a high of 0.31% nickel with average values >0.20% nickel (see table 4a).
Drilling conducted by Tres-Or Resources Ltd., did not report nickel assays but did intersect wide sections of serpentinized peridotite with magnetite and/or sulphide minerals (e.g., MAN-87-1) as observed in 22 drill holes (see Table 4b), as well as elevated PGM values (e.g., 0.57-0.59 g/t PGM) from several channel samples. Geological descriptions and geochemistry from these programs resemble what is observed at
Table 4a – Historical Drilling – Mann Northwest Property – Significant Intersections
Hole ID | From (m) | To (m) | Length (m) | Ni % | S % | Cr % | Co % | Pd (g/t) | Pt (g/t) |
FHR01-02 | 25.3 | 29.0 | 3.7 | 0.22 | 0.06 | 0.20 | 0.01 | 0.001 | - |
FHR01-02 | 73.0 | 76.0 | 3.0 | 0.21 | 0.07 | 0.11 | 0.01 | - | - |
FHR01-02 | 86.0 | 89.0 | 3.0 | 0.23 | 0.06 | 0.08 | 0.01 | 0.002 | - |
FHR01-02 | 89.0 | 92.3 | 3.3 | 0.24 | 0.05 | 0.07 | 0.01 | 0.002 | - |
FHR01-02 | 92.6 | 95.0 | 2.4 | 0.23 | 0.05 | 0.06 | 0.01 | 0.003 | - |
FHR01-02 | 98.0 | 101.0 | 3.0 | 0.24 | 0.05 | 0.06 | 0.01 | 0.002 | 0.007 |
FHR01-02 | 101.0 | 104.0 | 3.0 | 0.23 | 0.05 | 0.08 | 0.01 | 0.001 | - |
FHR01-02 | 131.0 | 134.0 | 3.0 | 0.25 | 0.04 | 0.08 | 0.01 | 0.002 | 0.007 |
FHR02-02 | 33.5 | 35.0 | 1.5 | 0.22 | 0.07 | 0.23 | 0.01 | 0.063 | 0.048 |
FHR02-02 | 75.4 | 76.4 | 1.0 | 0.21 | 0.10 | 0.14 | 0.01 | 0.003 | - |
FHR02-02 | 113.0 | 114.3 | 1.3 | 0.31 | 0.17 | 0.10 | 0.02 | 0.021 | 0.013 |
FHR02-02 | 117.0 | 118.6 | 1.6 | 0.21 | 0.09 | 0.08 | 0.01 | 0.002 | - |
FHR02-02 | 121.7 | 122.3 | 0.6 | 0.29 | 0.12 | 0.15 | 0.01 | 0.038 | 0.017 |
FHR02-02 | 134.7 | 135.4 | 0.7 | 0.28 | 0.19 | 0.19 | 0.01 | 0.044 | 0.021 |
FHR02-02 | 158.0 | 161.0 | 3.0 | 0.27 | 0.14 | 0.07 | 0.01 | 0.031 | 0.009 |
FHR03-02 | 27.5 | 32.0 | 4.5 | 0.17 | 0.10 | 0.08 | 0.01 | 0.004 | 0.014 |
FHR03-02 | 133.0 | 137.0 | 4.0 | 0.15 | 0.18 | 0.18 | 0.01 | 0.005 | - |
Table 4b – Historical Drilling – Mann Northwest Property – Selected Lithologies
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
FHR01-02 | 25.3 | 63.5 | 38.2 | Peridotite |
FHR01-02 | 63.5 | 87.5 | 24.0 | Peridotite |
FHR01-02 | 87.5 | 92.3 | 4.8 | Peridotite |
FHR01-02 | 92.6 | 111.8 | 19.2 | Peridotite |
Table 4b – Historical Drilling – Mann Northwest Property – Selected Lithologies (continued)
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
FHR01-02 | 116.9 | 119.1 | 2.2 | Peridotite |
FHR01-02 | 119.1 | 137.0 | 17.9 | Peridotite |
FHR02-02 | 7.0 | 33.5 | 26.5 | Peridotite |
FHR02-02 | 33.7 | 43.5 | 9.8 | Peridotite |
FHR02-02 | 43.5 | 150.0 | 106.5 | Peridotite |
FHR02-02 | 150.8 | 161.0 | 10.2 | Peridotite |
FHR03-02 | 15.0 | 123.8 | 108.8 | Peridotite |
MAN-73-6 | 12.2 | 112.3 | 100.1 | Peridotite |
MAN-73-6 | 115.5 | 119.9 | 4.4 | Peridotite |
MAN-73-6 | 119.9 | 128.0 | 8.1 | Pyroxenite |
MAN-73-6 | 152.1 | 167.6 | 15.5 | Peridotite |
MAN-00-01 | 5.2 | 100.3 | 95.1 | Peridotite |
MAN-00-01 | 100.3 | 104.0 | 3.8 | Gabbro |
MAN-00-01 | 104.0 | 106.5 | 2.4 | Peridotite |
MAN-00-01 | 106.5 | 128.8 | 22.3 | Gabbro |
MAN-00-01 | 128.8 | 200.3 | 71.5 | Peridotite |
MAN-01 | 5.2 | 100.3 | 95.1 | Peridotite |
MAN-01 | 100.3 | 104.0 | 3.8 | Gabbro |
MAN-01 | 104.0 | 106.5 | 2.4 | Peridotite |
MAN-01 | 106.5 | 128.8 | 22.3 | Gabbro |
MAN-01 | 128.8 | 200.3 | 71.5 | Peridotite |
M-01-1 | - | 192.0 | 192.0 | Peridotite |
M-01-2 | - | 212.3 | 212.3 | Gabbro |
M-01-2 | 212.3 | 237.1 | 24.8 | |
M-01-2 | 237.1 | 251.0 | 13.9 | Peridotite |
M-01-3 | - | 150.0 | 150.0 | Peridotite |
M-01-4 | - | 102.0 | 102.0 | Peridotite |
M-01-5 | - | 40.2 | 40.2 | Peridotite |
M-01-5 | 40.2 | 59.8 | 19.6 | Gabbro |
M-01-5 | 59.8 | 73.6 | 13.8 | Pyroxenite |
M-01-5 | 73.6 | 116.9 | 43.3 | Gabbro |
M-01-5 | 116.9 | 150.0 | 33.1 | Peridotite |
M-01-6 | - | 51.6 | 51.6 | Peridotite |
M-01-6 | 51.6 | 70.2 | 18.6 | Gabbro |
M-01-6 | 70.2 | 81.5 | 11.3 | Pyroxenite |
M-01-6 | 81.5 | 107.9 | 26.4 | Gabbro |
M-01-6 | 107.9 | 147.5 | 39.6 | Peridotite |
Table 4b – Historical Drilling – Mann Northwest Property – Selected Lithologies (continued)
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
M-01-6 | 147.5 | 156.0 | 8.5 | Gabbro |
MAN-87-1 | - | 9.7 | 9.7 | Gabbro |
MAN-87-1 | 9.7 | 41.2 | 31.4 | Peridotite |
MAN-87-2 | - | 11.6 | 11.6 | Gabbro |
MAN-87-2 | 11.6 | 35.4 | 23.8 | Peridotite |
MAN-88-1 | - | 61.6 | 61.7 | Peridotite |
MAN-88-1 | 61.6 | 64.0 | 2.4 | Gabbro |
MAN-88-2 | - | 61.0 | 61.0 | Peridotite |
MAN-88-3 | - | 60.7 | 60.7 | Peridotite |
MAN-91-1 | 1.8 | 79.6 | 77.7 | Gabbro |
MAN-91-1 | 79.6 | 138.9 | 59.4 | Peridotite |
MAN-91-1 | 138.9 | 155.5 | 16.6 | Gabbro |
MAN-91-1 | 155.5 | 166.2 | 10.7 | Gabbro |
MAN-91-1 | 166.2 | 181.9 | 15.7 | Pyroxenite |
MAN-91-1 | 181.9 | 246.0 | 64.1 | Peridotite |
MAN-96-1 | 1.5 | 42.1 | 40.5 | Gabbro |
MAN-96-1 | 42.1 | 107.3 | 65.2 | Peridotite |
MAN-96-1 | 107.3 | 115.2 | 7.9 | Pyroxenite |
MAN-96-1 | 115.2 | 227.1 | 111.9 | Peridotite |
MAN-96-1 | 227.1 | 248.7 | 21.6 | Pyroxenite |
MAN-96-1 | 248.7 | 279.8 | 31.2 | Peridotite |
MAN52-02 | 96.6 | 179.0 | 82.4 | Ultramafic |
MAN07-01 | 6.4 | 37.8 | 31.4 | Peridotite |
MAN07-01 | 37.8 | 47.7 | 9.9 | Gabbro |
MAN07-01 | 47.7 | 53.5 | 5.8 | Pyroxenite |
MAN07-01 | 53.5 | 76.7 | 23.2 | Gabbro |
MAN07-01 | 76.7 | 102.0 | 25.3 | Peridotite |
MAN07-02 | 14.2 | 30.0 | 15.8 | Pyroxenite |
MAN07-02 | 30.0 | 110.0 | 80.1 | Gabbro |
MAN07-02 | 110.0 | 129.0 | 19.0 | Peridotite |
MAN07-03 | 40.5 | 41.9 | 1.4 | Gabbro |
MAN07-03 | 41.9 | 61.7 | 19.8 | Peridotite |
MAN07-03 | 61.7 | 82.0 | 20.3 | Pyroxenite |
MAN07-03 | 82.0 | 107.3 | 25.3 | Peridotite |
MAN07-04 | 9.0 | 21.5 | 12.5 | Peridotite |
MAN07-04 | 21.5 | 22.3 | 0.8 | Pyroxenite |
MAN07-04 | 22.3 | 76.8 | 54.5 | Gabbro |
Table 4b – Historical Drilling – Mann Northwest Property – Selected Lithologies (continued)
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
MAN07-04 | 76.8 | 141.0 | 64.2 | Peridotite |
MAN08-05 | 14.5 | 26.9 | 12.4 | Pyroxenite |
MAN08-05 | 26.9 | 60.0 | 33.1 | Gabbro |
MAN08-06 | 13.0 | 25.8 | 12.8 | Peridotite |
MAN08-06 | 25.8 | 38.3 | 12.5 | Pyroxenite |
MAN08-06 | 38.3 | 60.0 | 21.7 | Gabbro |
MAN08-07 | 16.0 | 33.9 | 17.9 | Peridotite |
MAN08-07 | 33.9 | 46.3 | 12.4 | Pyroxenite |
MAN08-07 | 46.3 | 54.0 | 7.7 | Gabbro |
MAN08-07 | 54.0 | 57.5 | 3.5 | Pyroxenite |
MAN08-07 | 57.5 | 75.0 | 17.5 | Gabbro |
Figure 4 – Mann Northwest Property – Historical Drillholes Over TMI.
Mann Southeast
Mann Southeast is characterized by an arcuate-shaped ultramafic intrusion located in southeast Mann township with approximate dimensions of 6.2 km long and up to 800 metres wide (see Figure 5). Eight widely spaced holes drilled into the anomaly outlined 5 km of serpentinized dunite / peridotite across the anomaly (see Table 5c below).
In 1996,
A drill program conducted in 1973 around the southeast Mann ultramafic intersected wide intervals of serpentinized peridotite in five holes, with assays ranging up to 0.29% nickel (see Table 5b below). The southernmost and largest section of ultramafic – 1.2 km by 800 metres – remains untested with no historical drilling reported.
Table 5a – Historical Drilling – Mann Southeast Property – Significant Intersections
Hole ID | From (m) | To (m) | Ni % |
MAN-35-01 | 47.0 | 50.0 | 0.33 |
MAN-35-01 | 71.0 | 74.0 | 0.32 |
MAN-35-01 | 101.0 | 104.0 | 0.31 |
Table 5b – Historical Drilling – Mann Southeast Property – Significant Intersections
Hole ID | From (m) | To (m) | Ni % |
73-1 | 41.1 | 42.7 | 0.25 |
73-1 | 73.2 | 74.8 | 0.23 |
73-1 | 86.7 | 88.4 | 0.22 |
73-1 | 103.6 | 105.2 | 0.24 |
73-1 | 120.4 | 121.9 | 0.23 |
73-1 | 137.2 | 138.7 | 0.22 |
73-1 | 153.9 | 155.4 | 0.25 |
73-3 | 41.1 | 42.7 | 0.25 |
73-3 | 56.4 | 57.9 | 0.28 |
73-3 | 73.2 | 74.7 | 0.18 |
73-3 | 88.4 | 89.9 | 0.16 |
73-3 | 103.6 | 105.2 | 0.20 |
73-3 | 120.4 | 121.9 | 0.25 |
73-3 | 136.2 | 137.8 | 0.29 |
73-3 | 150.9 | 152.1 | 0.29 |
73-4 | 69.2 | 70.7 | 0.28 |
73-4 | 86.0 | 87.5 | 0.23 |
73-4 | 103.6 | 105.2 | 0.23 |
73-4 | 120.4 | 121.9 | 0.23 |
73-4 | 137.5 | 139.0 | 0.29 |
73-6 | 61.6 | 63.1 | 0.27 |
73-6 | 76.2 | 77.7 | 0.23 |
73-6 | 94.5 | 96.0 | 0.23 |
73-6 | 99.1 | 100.6 | 0.22 |
*Hole 73-2 had assays all below 0.15% |
Table 5c – Historical Drilling – Mann Southeast – Selected Lithologies
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
73-1 | 38.4 | 159.7 | 121.3 | Peridotite |
73-2 | 39.9 | 166.7 | 126.8 | Peridotite |
73-3 | 36.6 | 152.1 | 115.5 | Peridotite |
73-4 | 55.2 | 64.9 | 9.8 | Peridotite |
73-4 | 64.9 | 144.5 | 79.6 | Peridotite |
73-6 | 12.8 | 48.5 | 35.7 | Peridotite |
73-6 | 48.5 | 112.5 | 64.0 | Peridotite |
MAN-35-01 | 38.0 | 149.0 | 111.0 | Dunite |
MAN-45-01 | 99.0 | 155.0 | 56.0 | Peridotite |
MAN-45-01 | 195.0 | 245.0 | 50.0 | Peridotite |
MAN-45-02 | 95.0 | 211.0 | 116.0 | Peridotite |
Figure 5 – Mann Southeast Property – Historical Drillholes Over TMI.
Reaume
Reaume is a property approximately 5,800 ha located 54 km north-northeast of
Seven drillholes by
Four of the
Figure 6 – Reaume Property – Historical Drillholes Over TMI.
Table 6 – Historical Drilling – Reaume Property – Selected Lithologies
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
28483 | 37.0 | 89.0 | 52.0 | Peridotite |
28483 | 89.0 | 147.0 | 58.0 | Peridotite |
28483 | 147.0 | 301.0 | 154.0 | Peridotite/Dunite |
28482 | 140.0 | 158.0 | 18.0 | Peridotite/Dunite |
28482 | 158.0 | 248.0 | 90.0 | Peridotite |
REA-45-03 | 21.0 | 89.0 | 68.0 | Peridotite |
REA-45-03 | 89.0 | 117.0 | 28.0 | Pyroxenite |
REA-45-03 | 117.0 | 164.0 | 47.0 | Peridotite |
REA-45-03 | 164.0 | 198.0 | 34.0 | Pyroxenite |
REA-45-03 | 198.0 | 278.0 | 80.0 | Peridotite |
REA-45-03 | 294.0 | 335.0 | 41.0 | Pyroxenite |
REA-45-04 | 29.0 | 99.0 | 70.0 | Dunite |
Table 6 – Historical Drilling – Reaume Property – Selected Lithologies (continued)
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
REA-45-04 | 101.1 | 156.5 | 55.4 | Dunite |
REA-45-04 | 160.3 | 198.5 | 38.3 | Peridotite |
REA-45-04 | 198.5 | 344.9 | 146.4 | Dunite |
REA-45-05 | 30.0 | 123.8 | 93.8 | Dunite |
REA-45-05 | 123.8 | 223.1 | 99.3 | Peridotite |
REA-45-05 | 238.6 | 244.4 | 5.8 | Pyroxenite |
REA-45-05 | 244.4 | 293.0 | 48.6 | Peridotite |
REA-45-05 | 293.0 | 300.6 | 7.6 | Dunite |
REA-45-05 | 300.6 | 308.0 | 7.4 | Peridotite |
REA-45-06 | 21.7 | 320.0 | 298.3 | Peridotite |
REA-45-07 | 45.2 | 131.1 | 85.9 | Peridotite |
REA-45-07 | 131.1 | 299.0 | 167.9 | Dunite |
REA-45-08 | 33.0 | 54.5 | 21.5 | Dunite |
REA-45-08 | 54.5 | 64.4 | 9.9 | Pyroxenite |
REA-46-01 | 15.0 | 28.4 | 13.4 | Dunite |
REA-46-01 | 28.4 | 136.8 | 108.4 | Dunite |
REA-46-01 | 136.8 | 259.5 | 122.7 | Peridotite |
REA-46-01 | 259.5 | 310.0 | 50.5 | Pyroxenite |
REA-46-01 | 310.0 | 337.9 | 27.9 | Peridotite |
REA-46-01 | 350.3 | 388.5 | 38.2 | Pyroxenite |
REA-46-01 | 388.5 | 419.4 | 30.9 | Peridotite |
Midlothian
Midlothian covers an area of 3,257 ha and is located 70 km south-southeast of
A total of 30 holes were drilled over the last 50 years by various operators with 23 holes intersecting serpentinized peridotite/dunite and 17 ending while still in the ultramafics. Six drillholes, each intersected over 100 metres of continuous, uninterrupted dunite/ultramafic, with LM08-01 intersecting 263.8 metres to the end of hole. (See Table 7a).
Seven holes had nickel assays, with the best interval in hole LM08-01 which yielded 0.24% nickel across core length of 345 metres with the final 42 metres grading 0.30% nickel (See Table 7b). Nickel sampling was not continuous down most drillholes.
The above drillholes outline serpentinized dunite/peridotite over a strike distance of 3.1 km long by 670 metres wide.
Figure 7 – Midlothian Property – Historical drillholes over TMI.
Table 7a – Historical Drilling – Midlothian Property – Selected Lithologies
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
LM08-01 | 51.6 | 60.2 | 8.6 | Peridotite/dunite |
LM08-01 | 60.2 | 135.8 | 75.7 | Serpentinite |
LM08-01 | 136.4 | 400.2 | 263.8 | Peridotite/dunite |
LL1 | 7.0 | 165.8 | 158.8 | Dunite |
LL2 | 8.8 | 163.1 | 154.3 | Dunite |
LL3 | 9.8 | 160.0 | 150.3 | Dunite |
A-121 | 2.7 | 48.8 | 46.0 | Dunite |
A-126 | 7.6 | 37.2 | 29.6 | Dunite |
A-126 | 41.8 | 92.0 | 50.3 | Dunite |
A-126 | 92.7 | 152.7 | 60.1 | Dunite |
501 | 133.2 | 196.3 | 63.1 | Dunite |
506 | 206.0 | 301.8 | 95.7 | Dunite |
507 | 106.1 | 280.7 | 174.7 | Dunite |
A-131 | 0.9 | 13.1 | 12.2 | Dunite |
A-131 | 36.6 | 39.9 | 3.4 | Dunite |
A-131 | 102.7 | 106.7 | 4.0 | Dunite |
A-131 | 110.9 | 113.1 | 2.1 | Dunite |
503 | 3.7 | 20.4 | 16.8 | Dunite |
504 | 6.7 | 114.0 | 107.3 | Dunite |
Table 7a – Historical Drilling – Midlothian Property – Selected Lithologies (continued)
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
MD-17-001 | 20.5 | 20.5 | 0.0 | Serpentinite |
MD-17-001 | 20.5 | 26.1 | 5.6 | Serpentinite |
MD-17-001 | 26.1 | 29.0 | 2.9 | Dunite |
MD-17-002 | 20.0 | 29.0 | 9.0 | Serpentinite |
MD-17-003 | 0.0 | 31.1 | 31.1 | Serpentinite |
MD-17-003 | 0.0 | 35.0 | 35.0 | Dunite |
MD-17-004 | 18.4 | 19.9 | 1.5 | Dunite |
MD-17-005 | 41.0 | 53.0 | 12.0 | Dunite |
MD-17-006 | 32.0 | 38.0 | 6.0 | Dunite |
MD-17-007 | 28.8 | 35.0 | 6.2 | Serpentinite |
MD-17-007 | 35.0 | 67.0 | 32.0 | Dunite |
MD-17-008 | 29.3 | 38.0 | 8.8 | Serpentinite |
514 | 45.9 | 52.1 | 6.2 | Dunite |
514 | 52.1 | 70.7 | 18.6 | Dunite |
514 | 70.7 | 92.7 | 21.9 | Dunite |
514 | 92.7 | 107.3 | 14.6 | Dunite |
514 | 117.7 | 149.4 | 31.7 | Dunite |
515 | 32.6 | 33.8 | 1.2 | Dunite |
515 | 33.8 | 78.3 | 44.5 | Peridotite/dunite |
515 | 78.3 | 86.3 | 7.9 | Dunite |
515 | 86.3 | 125.6 | 39.3 | Peridotite/dunite |
515 | 125.6 | 143.3 | 17.7 | Dunite |
516 | 48.5 | 84.7 | 36.3 | Peridotite/dunite |
516 | 92.0 | 105.2 | 13.1 | Dunite |
516 | 107.9 | 119.8 | 11.9 | Peridotite/dunite |
516 | 119.8 | 137.2 | 17.4 | Dunite |
Table 7b – Historical Drilling – Midlothian Property – Significant Intersections
Hole ID | From (m) | To (m) | Length (m) | Ni % |
LM08-01 | 52.0 | 397.0 | 345.0 | 0.24 |
including | 352.0 | 397.0 | 45.0 | 0.30 |
Reid
The Reid Property is located 16 km southwest of Crawford and covers an area of 3,800 ha. The property contains a series of folded ultramafic bodies that measure 3.3 km north-south by 2.1 km east-west based on the TMI. See Figure 8.
Only four holes were ever drilled inside or near the edge of the ultramafic (from 1966 to 1972) by three different companies. All four holes collared and ended in ultramafic rocks with the holes ending at depths of 59.7-171.0 metres with intervals of ultramafics ranging from 44.5-123.7 metres. While none of the holes were assayed, all four holes intersected peridotite with up to 5-10% disseminated magnetite noted in each hole (see Table 8 below).
Table 8 – Historical Drilling – Reid Property – Selected Lithologies
Hole ID | From (m) | To (m) | Rock Type |
R-22 | 29.0 | 106.7 | Serpentinized gabbro to peridotite |
R-22 | 125.0 | 171.0 | Serpentinized peridotite |
R-18 | 54.6 | 96.9 | Peridotite |
T67-1 | 20.7 | 128.3 | Serpentinized peridotite |
T67-2 | 15.2 | 59.7 | Serpentinized peridotite |
Figure 8 – Reid Property – Historical Drillholes Over TMI.
Table 9 – Historical Drilling – Adam McCool Property – Selected Lithologies
Hole ID | From (m) | To (m) | Length (m) | Rock Type |
1-63 | 33.5 | 121.9 | 88.1 | Serpentinized Dunite |
1-62 | 38.1 | 150.9 | 112.8 | Serpentinized Dunite |
1-63 | 3.0 | 33.8 | 30.8 | Serpentinized Dunite |
1586-1 | 48.6 | 139.7 | 91.1 | Peridotite |
1586-1 | 139.7 | 153.3 | 13.6 | Gabbro |
D-1 | 29.3 | 279.5 | 250.2 | Serpentinite |
Figure 9 – Adam McCool Property – Historical Drillholes Over TMI.
Powell
The Powell Property is located 74 km southeast of
Figure 10 – Powell Property – Historical Drillholes Over TMI.
Moody
The Moody Property covers an area of 1,940 ha and was staked by
Figure 11 – Moody Property – Historical Drillholes Over TMI.
Mortimer
The Mortimer Property includes two ultramafic intrusions that cover a total distance of 10 km, in an area staked by
Figure 12 – Mortimer Property – Historical Drillholes Over TMI.
Stimson
The Stimson Property covers 1,491 ha and encompasses a weakly magnetic ultramafic having a strike length of at least 2 km and with a higher amplitude TMI of 400 metres long. The ultramafic is interpreted to be a more distal extension of more strongly magnetic ultramafics found in Mortimer and Moody Townships, staked by
Figure 13 – Stimson Property – Historical Drillholes Over TMI.
Purchase and Option Agreements
The Company has negotiated 18 agreements to acquire the properties described in the release. On signing, the Company will pay a combined
Table 10 – Consolidated Summary of Cash & Share Consideration: 18 transactions
Cash | Shares | |
On Signing | 2,044,000 | |
Year 1 | 926,000 | |
Year 2 | 35,000 | |
Year 3 | 425,000 | |
Year 4 | 140,000 | |
Total | 3,570,000 |
Sothman
Mann
The Mann Property was acquired from Noble Mineral Exploration ("Noble") in an Option Agreement with work commitments, cash payments, share issuances, NSRs, and buy-back provisions. The Company has acquired the right to earn an 80% interest in the Mann Property from Noble. Work commitments are
Reaume
The Reaume Property was acquired through a combination of Purchase and Option Agreements. In one Purchase Agreement Canada Nickel acquired a 100% right to 65 contiguous mining claims with a 2.00% NSR to the vendor and a 1.00% buy-back provision. In a second Option Agreement Canada Nickel has the option to earn a 100% interest in 48 mining claims through work expenditures (2,100 metres of diamond drilling) over a 12-month period. In a third Purchase Agreement Canada Nickel acquired a 100% interest in a group of 201 in-fill claims (surrounding the ultramafic units) with the vendor retaining a 2.00% NSR with a buy-back of 1.00%. In a fourth Purchase Agreement Canada Nickel acquired a small group of claims which have a 2.00% NSR with a 1.00% buy-back.
Midlothian
The Midlothian Property was acquired under an Option Agreement with
Reid
The Reid Property was acquired through Purchase Agreements with several different vendors. The Company has committed to conduct a 2,500 m drill program and fly an airborne survey over the Property. The vendor retains a 2.00% NSR on the claims with certain buy-down provisions. In a second Purchase Agreement 14 single cell mining claims were acquired with a 2.00% NSR to the vendor and a 1.00% buy-back. In a third agreement
The Adam McCool Property was staked directly by
Powell
The Powell Property was acquired through a Purchase Agreement with a single vendor. The vendor retains a 2.00% NSR with a 1.00% buy-back for
Stimson-Mortimer-Moody
The Stimson,
Additional Land Acquisition - Kingsmill and Mabee Townships
The Company has agreed to acquire the remaining patents in Kingsmill and Mabee township covering approximately 15,000 hectares from Noble Mineral Exploration in exchange for 500,000 shares of the Company.
Statement Regarding TSX Venture
Neither
The completion of any transactions mentioned in this release is subject to customary closing conditions, including final
Statement Regarding Historical Resource Estimates
The Sothman historical resource estimate is unclassified and does not comply with CIM Definition Standards on Mineral Resources and Mineral Reserves as required by NI 43-101. The historical resource was reported by
Qualified Person and Data Verification
Conference Call Details
Date:
Time:
Participants may join the call as follows:
Dialing local
Dialing North American Toll Free: +1-888-390-0546
Dialing International Toll Free: available upon request
Webcast URL:
https://produceredition.webcasts.com/starthere.jsp?ei=1514838&tp_key=41b4857d60
Confirmation #: 94728691
For those unable to participate, a web-based archive of the conference call will be available for playback at the same Audience URL used to access the live webcast. Also, an audio replay will be available from
About
For further information, please contact:
Chair and CEO
Phone: 647-256-1954
Email: info@canadanickel.com
Cautionary Statement Concerning Forward-Looking Statements
This press release contains certain information that may constitute "forward-looking information" under applicable Canadian securities legislation. Forward looking information includes, but is not limited to, drill and exploration results relating to the target properties described herein (the "Properties"), the potential of the
Appendix
Table A – Collars
Hole ID | Property | Northing | Easting | Azimuth | Dip | Length |
(mN-NAD27) | (mE-NAD27) | (o) | (o) | (m) | ||
SM56-K11 | Sothman West | 5,299,305.0 | 481,535.0 | 180 | -60 | 148.4 |
SM67-B06 | Sothman West | 5,299,281.8 | 481,575.8 | 180 | -45 | 101.8 |
DG50-S04 | Sothman West | 5,299,235.0 | 481,714.0 | 131 | -45 | 107.9 |
DG51-S20 | Sothman West | 5,299,112.9 | 481,750.5 | 0 | -48 | 111.0 |
DG50-S05 | Sothman West | 5,299,224.0 | 481,767.0 | 180 | -45 | 82.0 |
SM71-01 | Sothman West | 5,299,404.0 | 481,638.0 | 180 | -68 | 426.7 |
SM71-02 | Sothman West | 5,299,385.0 | 481,487.0 | 180 | -63 | 366.7 |
SM67-B25 | Sothman | 5,299,144.5 | 482,936.8 | 207 | -45 | 91.2 |
SM67-B26 | Sothman | 5,299,069.3 | 482,692.9 | 207 | -45 | 120.1 |
SM67-B27 | Sothman | 5,299,007.8 | 482,659.2 | 200 | -45 | 121.6 |
SM67-B28 | Sothman | 5,298,937.8 | 482,650.8 | 191 | -45 | 107.9 |
DG51-S12 | Sothman | 5,298,954.6 | 482,617.8 | 180 | -45 | 148.4 |
DG51-S09 | Sothman | 5,299,124.3 | 482,107.5 | 206 | -44 | 229.8 |
DG53-S41A | Sothman | 5,298,932.2 | 483,982.2 | 175 | -55 | 83.8 |
FY-02-01 | 5,361,223.0 | 480,883.0 | 270 | -45 | 102.0 | |
FY-02-02 | 5,361,232.0 | 480,387.0 | 223 | -40 | 472.0 | |
FY-02-03 | 5,360,750.0 | 481,376.0 | 180 | -45 | 100.0 | |
FY-02-04 | 5,360,987.0 | 481,945.0 | 345 | -45 | 147.0 | |
FY-02-05 | 5,361,019.0 | 482,117.0 | 343 | -50 | 172.0 | |
FY-02-06 | 5,361,309.0 | 480,561.0 | 100 | -45 | 301.0 | |
FY-02-07 | 5,361,678.0 | 481,022.0 | 70 | -45 | 77.0 | |
FY-02-08 | 5,361,629.0 | 481,012.0 | 75 | -45 | 77.0 | |
FY-02-09 | 5,361,564.0 | 480,990.0 | 82 | -45 | 125.0 | |
FY-02-10 | 5,361,124.0 | 480,240.0 | 37 | -45 | 135.0 | |
FY-02-11 | 5,361,216.0 | 480,192.0 | 22 | -45 | 115.0 | |
FY-02-12 | 5,361,085.0 | 480,267.0 | 55 | -45 | 272.0 | |
FY-02-13 | 5,361,161.0 | 480,224.0 | 60 | -60 | 318.0 | |
1A | Mann Central | 5,410,706.6 | 498,457.0 | 180 | -60 | 57.9 |
2A | Mann Central | 5,410,850.6 | 498,694.2 | 180 | -50 | 128.7 |
3A | Mann Central | 5,410,906.2 | 498,782.2 | 180 | -45 | 80.6 |
4A | Mann Central | 5,410,641.2 | 498,291.4 | 180 | -70 | 37.5 |
INCO-1 | Mann Central | 5,409,763.7 | 497,819.1 | 180 | -45 | 162.5 |
M-1 | Mann Central | 5,410,084.4 | 497,893.6 | 360 | -45 | 213.7 |
M-2 | Mann Central | 5,410,312.5 | 496,873.2 | 180 | -45 | 214.9 |
M-3 | Mann Central | 5,410,447.3 | 496,891.5 | 180 | -45 | 172.9 |
M-4 | Mann Central | 5,410,662.2 | 496,900.1 | 180 | -45 | 213.1 |
Table A – Collars (continued)
Hole ID | Property | Northing | Easting | Azimuth | Dip | Length |
M-5 | Mann Central | 5,410,675.8 | 496,672.5 | 180 | -45 | 172.6 |
M-6 | Mann Central | 5,410,454.5 | 496,683.0 | 180 | -45 | 128.1 |
M-7 | Mann Central | 5,410,788.5 | 495,884.3 | 180 | -45 | 172.9 |
M-8 | Mann Central | 5,410,852.2 | 495,864.3 | 360 | -45 | 172.0 |
MA4-1-76 | Mann Central | 5,410,846.5 | 499,368.3 | 180 | -50 | 134.2 |
MA4-2-76 | Mann Central | 5,410,725.8 | 499,366.5 | 180 | -50 | 123.2 |
MA5-1-76 | Mann Central | 5,410,722.7 | 498,551.2 | 180 | -50 | 138.1 |
MA5-2-76 | Mann Central | 5,410,108.0 | 498,351.5 | 180 | -50 | 123.2 |
MAN43-01 | Mann Central | 5,410,157.8 | 498,349.5 | 360 | -45 | 188.0 |
MAN43-02 | Mann Central | 5,410,255.4 | 499,225.2 | 180 | -45 | 113.0 |
MAN43-03 | Mann Central | 5,410,152.9 | 498,539.9 | 180 | -45 | 158.0 |
MN87-3 | Mann Central | 5,410,577.1 | 498,394.2 | 360 | -50 | 151.2 |
87-01 | Mann NW | 5,412,224.9 | 494,853.7 | 270 | -65 | 41.2 |
87-02 | Mann NW | 5,412,225.6 | 494,853.7 | 270 | -80 | 35.4 |
79-01 | Mann NW | 5,413,332.9 | 495,724.4 | 190 | -55 | 133.5 |
91-01 | Mann NW | 5,411,924.9 | 494,887.1 | 120 | -48 | 246.0 |
FHR01-02 | Mann NW | 5,412,461.5 | 495,870.1 | 215 | -45 | 137.0 |
FHR02-02 | Mann NW | 5,412,192.5 | 495,873.8 | 215 | -45 | 161.0 |
FHR03-02 | Mann NW | 5,413,542.5 | 496,596.6 | 215 | -45 | 170.0 |
H-88-1 | Mann NW | 5,412,164.8 | 494,936.1 | 225 | -50 | 64.0 |
H-88-2 | Mann NW | 5,412,162.3 | 494,936.1 | 225 | -65 | 61.0 |
H-88-3 | Mann NW | 5,412,162.6 | 494,937.2 | 225 | -40 | 60.7 |
M-01-1 | Mann NW | 5,412,280.0 | 494,630.5 | 70 | -45 | 192.0 |
M-01-2 | Mann NW | 5,411,887.5 | 494,880.9 | 55 | -45 | 251.0 |
M-01-3 | Mann NW | 5,412,117.0 | 494,683.2 | 280 | -45 | 150.0 |
M-01-4 | Mann NW | 5,412,080.0 | 494,686.2 | 45 | -45 | 102.0 |
M-01-5 | Mann NW | 5,412,164.0 | 494,771.6 | 240 | -45 | 150.0 |
M-01-6 | Mann NW | 5,412,156.9 | 494,787.6 | 240 | -70 | 150.0 |
M96-1 | Mann NW | 5,411,921.3 | 494,847.2 | 172 | -65 | 245.0 |
MAN-01 | Mann NW | 5,412,235.0 | 495,567.8 | 215 | -45 | 200.3 |
MAN07-01 | Mann NW | 5,412,468.0 | 494,789.0 | 280 | -50 | 102.0 |
MAN07-02 | Mann NW | 5,412,251.0 | 494,872.0 | 240 | -48 | 126.0 |
MAN07-03 | Mann NW | 5,412,319.1 | 494,754.0 | 270 | -48 | 108.0 |
MAN07-04 | Mann NW | 5,412,369.0 | 494,848.0 | 240 | -46 | 141.0 |
MAN08-05 | Mann NW | 5,412,251.0 | 494,872.0 | 240 | -48 | 60.0 |
MAN08-06 | Mann NW | 5,412,251.0 | 494,872.0 | 0 | -90 | 60.0 |
MAN08-07 | Mann NW | 5,412,251.0 | 494,872.0 | 300 | -48 | 75.0 |
MAN52-02 | Mann NW | 5,412,507.4 | 496,491.1 | 180 | -45 | 179.0 |
MAN-73-6 | Mann NW | 5,412,367.0 | 495,208.9 | 180 | -50 | 167.6 |
Table A – Collars (continued)
Hole ID | Property | Northing | Easting | Azimuth | Dip | Length |
MAN-73-6 | Mann NW | 5,412,358.5 | 494,887.8 | 180 | -50 | 167.6 |
MAN-87-1 | Mann NW | 5,412,274.6 | 494,791.6 | 270 | -65 | 41.2 |
MAN-87-1 | Mann NW | 5,412,375.5 | 494,775.7 | 270 | -65 | 41.2 |
MAN-87-2 | Mann NW | 5,412,251.0 | 494,793.5 | 270 | -80 | 35.4 |
MAN-87-2 | Mann NW | 5,412,356.1 | 494,776.2 | 270 | -80 | 35.4 |
MAN-88-1 | Mann NW | 5,412,098.9 | 494,880.2 | 235 | -50 | 64.0 |
MAN-88-1 | Mann NW | 5,412,077.5 | 494,846.5 | 235 | -50 | 64.0 |
MAN-88-2 | Mann NW | 5,412,070.5 | 494,878.4 | 235 | -65 | 61.0 |
MAN-88-2 | Mann NW | 5,412,044.5 | 494,842.1 | 235 | -65 | 61.0 |
MAN-88-3 | Mann NW | 5,412,046.0 | 494,872.6 | 235 | -40 | 60.7 |
MAN-88-3 | Mann NW | 5,412,015.5 | 494,843.9 | 235 | -40 | 60.7 |
MAN-91-1 | Mann NW | 5,411,812.0 | 494,843.2 | 120 | -48 | 246.0 |
MAN-91-1 | Mann NW | 5,411,815.5 | 494,866.9 | 120 | -48 | 246.0 |
MAN-96-1 | Mann NW | 5,411,779.5 | 494,862.6 | 172 | -65 | 279.8 |
MD-06-4 | Mann NW | 5,412,250.1 | 496,400.0 | 360 | -50 | 260.0 |
73-01 | Mann SE | 5,407,714.3 | 503,532.3 | 273 | -56 | 159.8 |
73-10 | Mann SE | 5,409,611.1 | 503,128.9 | 230 | -54 | 125.0 |
73-02 | Mann SE | 5,407,421.6 | 503,682.0 | 273 | -55 | 166.8 |
73-03 | Mann SE | 5,406,989.3 | 503,547.8 | 273 | -50 | 152.1 |
73-04 | Mann SE | 5,408,652.6 | 502,940.7 | 183 | -51 | 144.5 |
73-05 | Mann SE | 5,408,627.3 | 501,849.5 | 183 | -50 | 109.5 |
73-06 | Mann SE | 5,408,961.4 | 501,738.5 | 183 | -50 | 112.5 |
MAN35-01 | Mann SE | 5,408,387.8 | 503,614.6 | 220 | -45 | 149.0 |
MAN45-01 | Mann SE | 5,409,991.9 | 501,335.1 | 180 | -45 | 245.0 |
MAN45-02 | Mann SE | 5,409,950.4 | 501,605.7 | 180 | -45 | 211.3 |
MAN52-01 | Mann SE | 5,406,451.4 | 502,850.9 | 360 | -45 | 219.0 |
28482 | Reaume | 5,421,363.0 | 487,600.0 | 0 | -50 | 248.0 |
28483 | Reaume | 5,422,007.0 | 488,260.0 | 270 | -50 | 301.0 |
REA-45-04 | Reaume | 5,421,707.0 | 488,542.0 | 180 | -50 | 368.0 |
REA-45-05 | Reaume | 5,421,932.0 | 488,576.0 | 180 | -50 | 308.0 |
REA-45-06 | Reaume | 5,422,212.0 | 488,604.0 | 180 | -50 | 320.0 |
REA-45-07 | Reaume | 5,422,398.0 | 488,610.0 | 180 | -50 | 299.0 |
REA-45-08 | Reaume | 5,421,684.0 | 487,735.0 | 180 | -50 | 199.4 |
DH-01 | Reaume | 5,422,601.0 | 488,298.0 | 0 | -90 | 95.0 |
DH-02 | Reaume | 5,422,601.0 | 489,004.0 | 0 | -90 | 103.6 |
REA-45-03 | Reaume | 5,422,190.0 | 488,903.0 | 180 | -50 | 335.0 |
REA-46-01 | Reaume | 5,422,850.0 | 488,016.0 | 180 | -50 | 419.4 |
R-78-1 | Reaume | 5,421,678.0 | 486,639.0 | 210 | -45 | 49.7 |
LM08-01 | Midlothian | 5,303,260.0 | 499,195.0 | 180 | -50 | 400.2 |
Table A – Collars (continued)
Hole ID | Property | Northing | Easting | Azimuth | Dip | Length |
LL1 | Midlothian | 5,302,980.0 | 499,242.0 | 6 | -45 | 165.8 |
LL2 | Midlothian | 5,302,870.0 | 499,192.0 | 6 | -45 | 163.1 |
LL3 | Midlothian | 5,302,870.0 | 499,194.0 | 186 | -45 | 160.0 |
A-121 | Midlothian | 5,302,910.0 | 498,866.0 | 187 | -45 | 91.4 |
A-126 | Midlothian | 5,302,820.0 | 499,021.0 | 188 | -45 | 152.7 |
501 | Midlothian | 5,302,620.0 | 501,288.0 | 25 | -45 | 196.3 |
505 | Midlothian | 5,302,630.0 | 501,288.0 | 205 | -45 | 82.0 |
506 | Midlothian | 5,302,590.0 | 501,369.0 | 25 | -45 | 301.8 |
507 | Midlothian | 5,302,620.0 | 501,289.0 | 340 | -45 | 280.7 |
A-131 | Midlothian | 5,302,520.0 | 500,429.0 | 183 | -45 | 115.8 |
503 | Midlothian | 5,302,650.0 | 498,883.0 | 181 | -45 | 121.9 |
504 | Midlothian | 5,302,660.0 | 498,883.0 | 1 | -45 | 121.9 |
502 | Midlothian | 5,303,250.0 | 499,094.0 | 352 | -45 | 146.6 |
MD-17-008 | Midlothian | 5,303,230.0 | 499,727.0 | 280 | -50 | 38.0 |
MD-17-009 | Midlothian | 5,303,230.0 | 499,727.0 | 300 | -50 | 38.0 |
MD-17-007 | Midlothian | 5,303,230.0 | 499,727.0 | 220 | -50 | 67.0 |
MD-17-006 | Midlothian | 5,303,230.0 | 499,727.0 | 260 | -55 | 38.0 |
MD-17-005 | Midlothian | 5,303,230.0 | 499,727.0 | 260 | -89 | 53.0 |
MD-17-004 | Midlothian | 5,303,220.0 | 499,709.0 | 256 | -49 | 19.9 |
MD-17-003 | Midlothian | 5,303,220.0 | 499,709.0 | 220 | -84 | 35.0 |
MD-17-002 | Midlothian | 5,303,220.0 | 499,709.0 | 220 | -45 | 29.0 |
MD-17-001 | Midlothian | 5,303,220.0 | 499,709.0 | 220 | -60 | 29.0 |
LL6 | Midlothian | 5,303,020.0 | 499,770.0 | 185 | -45 | 166.4 |
516 | Midlothian | 5,303,350.0 | 502,009.0 | 360 | -45 | 137.2 |
515 | Midlothian | 5,303,350.0 | 502,014.0 | 0 | -90 | 150.3 |
514 | Midlothian | 5,303,180.0 | 502,010.0 | 0 | -90 | 154.5 |
LL7 | Midlothian | 5,302,990.0 | 498,825.0 | 187 | -50 | 160.7 |
LL4 | Midlothian | 5,303,120.0 | 499,410.0 | 185 | -45 | 164.6 |
LL5 | Midlothian | 5,303,020.0 | 499,030.0 | 187 | -45 | 165.9 |
R-22 | Reid | 5,403,720.0 | 456,699.0 | Grid W | -50 | 171.0 |
R-18 | Reid | 5,404,480.0 | 456,224.0 | Grid E | -50 | 96.9 |
T67-1 | Reid | 5,405,400.0 | 456,745.0 | 35 | -50 | 128.3 |
T67-2 | Reid | 5,405,510.0 | 456,709.0 | 210 | -49 | 59.7 |
1-63 | McCool | 5,384,613.0 | 566,975.6 | 360 | -85 | 122.0 |
2-63 | McCool | 5,383,250.0 | 566,050.3 | 35 | -60 | 188.0 |
3-63 | McCool | 5,384,550.8 | 567,035.3 | 0 | -90 | 150.9 |
1586-1 | McCool | 5,384,110.0 | 567,059.1 | 0 | -90 | 33.8 |
D-1 | McCool | 5,383,880.8 | 567,597.7 | 54 | -45 | 279.6 |
View original content to download multimedia:https://www.prnewswire.com/news-releases/canada-nickel-expands-timmins-nickel-district--acquires-13-additional-highly-prospective-nickel-properties-in-timmins-region-301429663.html
SOURCE
© Canada Newswire, source