VANCOUVER, BC, Nov. 30,
2022 /CNW/ - Power Metals
Corp. ("Power Metals" or the "Company")
(TSXV: PWM) (FRANKFURT:OAA1) (OTCQB:PWRMF) is pleased to announce
that drill holes have intersected lithium (Li), cesium (Cs) and
tantalum (Ta) mineralization with 20.25 % Cs2O, 1.29 %
Li2O and 147 ppm Ta over 1.0
m in drill hole PWM-22-150 in the West Joe Dyke, Case Lake
property, Cochrane, Ontario.
High-grade Li-Ta mineralization was also intersected: 3.10 %
Li2O, 0.09 % Cs2O and 841 ppm Ta over
2.0 m in drill hole PWM-22-149.
West Joe Dyke is a
three-commodity pegmatite with lithium (Li), cesium (Cs) and
tantalum (Ta) mineralization. The Ta mineralization occurs in the
aplite border zone, the spodumene zone and the pollucite zone. The
Li mineralization occurs in the spodumene zone and the pollucite
zone. The spodumene ranges in colour from pale green to white to
pink to purple in the spodumene zone. The Cs mineralization occurs
in the pollucite zone as a pod in the center of the West Joe
Dyke.
Lithium assay highlights on West Joe Dyke include (Table 1):
- 3.10 % Li2O, 0.09 % Cs2O and 841 ppm Ta,
25.0 – 27.0 m, 2.0 m interval, PWM-22-149 (Figure 1)
- 2.88 % Li2O, 1.31 % Cs2O and 682 ppm Ta,
20.0 – 22.0 m, 2.0 m interval, PWM-22-149
- 2.64 % Li2O, 0.08 % Cs2O and 730.6 ppm
Ta, 24.59 – 27.32 m, 2.73 m interval, PWM-22-149
- 2.56 % Li2O, 0.08 % Cs2O and 348 ppm Ta,
26.72 – 27.0 m, 0.28 m interval, PWM-22-156
Cesium assay highlights on the West Joe Dyke include (Table
1):
- 20.25 % Cs2O, 1.29 % Li2O and 147 ppm Ta,
31.0 – 32.0 m, 1.0 interval,
PWM-22-150 (Figure 2)
- 7.93 % Cs2O, 0.52 % Li2O and 129 ppm Ta,
22.0 – 22.67 m, 0.67 m interval, PWM-22-149
- 6.14 % Cs2O, 0.60 % Li2O and 150 ppm Ta,
18.0 – 18.70 m, 0.70 m interval, PWM-22-148
- 5.78 % Cs2O, 1.86 % Li2O and 522 ppm Ta,
32.0 – 33.0 m, 1.0 m interval, PWM-22-156
- 5.72 % Cs2O, 1.94 % Li2O and 862 ppm Ta,
27.76 – 32.0 m, 4.24 m interval, PWM-22-150
Tantalum assay highlights on the West Joe Dyke include (Table
1):
- 1613 ppm Ta, 1.53 % Li2O and 3.69 % Cs2O,
29.0 – 30.0 m, 1.0 m interval, PWM-22-156
- 1422 ppm Ta, 0.72 % Li2O and 0.03 % Cs2O,
34.53 – 35.0 m, 0.47 m interval, PWM-22-152
- 1156 ppm Ta, 2.30 % Li2O and 1.33 % Cs2O,
28.0 – 31.0 m, 3.0 m in interval, PWM-22-150 (Figure 2)
Table 1 Assay highlights from spodumene and pollucite zones,
West Joe Dyke, drill holes PWM-22-148 to 162.
Drill hole
#
|
including
|
From
(m)
|
To
(m)
|
Length
(m)
|
Li2O
(%)
|
Cs2O
(%)
|
Ta
(ppm)
|
PWM-22-148
|
|
15.85
|
18.70
|
2.85
|
1.35
|
1.69
|
195.89
|
PWM-22-148
|
including
|
18.00
|
18.70
|
0.70
|
0.60
|
6.14
|
150.00
|
PWM-22-148
|
|
19.41
|
22.82
|
3.41
|
1.36
|
0.28
|
190.25
|
PWM-22-149
|
|
19.65
|
22.67
|
3.02
|
2.11
|
2.63
|
494.88
|
PWM-22-149
|
including
|
20.00
|
22.00
|
2.00
|
2.88
|
1.31
|
682.00
|
PWM-22-149
|
including
|
22.00
|
22.67
|
0.67
|
0.52
|
7.93
|
129.00
|
PWM-22-149
|
|
23.26
|
23.89
|
0.63
|
0.68
|
4.23
|
641.00
|
PWM-22-149
|
|
24.59
|
27.32
|
2.73
|
2.64
|
0.08
|
730.60
|
PWM-22-149
|
including
|
25.00
|
27.00
|
2.00
|
3.10
|
0.09
|
841.00
|
PWM-22-150
|
|
27.76
|
32.00
|
4.24
|
1.94
|
5.72
|
862.33
|
PWM-22-150
|
including
|
28.00
|
31.00
|
3.00
|
2.30
|
1.33
|
1156.00
|
PWM-22-150
|
including
|
31.00
|
32.00
|
1.00
|
1.29
|
20.25
|
147.00
|
PWM-22-151
|
|
30.55
|
35.81
|
5.26
|
0.97
|
0.44
|
433.31
|
PWM-22-151
|
including
|
31.00
|
32.00
|
1.00
|
1.54
|
0.09
|
571.00
|
PWM-22-151
|
including
|
33.00
|
34.00
|
1.00
|
1.11
|
2.05
|
758.00
|
PWM-22-151
|
|
42.05
|
42.33
|
0.28
|
1.41
|
0.67
|
225.00
|
PWM-22-152
|
|
32.34
|
33.40
|
1.06
|
1.20
|
0.03
|
434.00
|
PWM-22-152
|
|
34.53
|
35.00
|
0.47
|
0.72
|
0.03
|
1422.00
|
PWM-22-153
|
|
46.20
|
49.20
|
3.00
|
1.24
|
0.06
|
358.91
|
PWM-22-153
|
including
|
47.00
|
48.77
|
1.77
|
1.45
|
0.06
|
354.59
|
PWM-22-154
|
|
49.73
|
50.84
|
1.11
|
1.58
|
0.05
|
195.00
|
PWM-22-155
|
|
62.63
|
63.63
|
1.00
|
0.58
|
0.37
|
2.70
|
PWM-22-156
|
including
|
26.72
|
27.00
|
0.28
|
2.56
|
0.08
|
348.00
|
PWM-22-156
|
|
26.72
|
34.07
|
7.35
|
1.44
|
1.87
|
571.61
|
PWM-22-156
|
including
|
29.00
|
30.00
|
1.00
|
1.53
|
3.69
|
1613.00
|
PWM-22-156
|
including
|
31.00
|
32.00
|
1.00
|
2.02
|
0.04
|
59.10
|
PWM-22-156
|
including
|
32.00
|
33.00
|
1.00
|
1.86
|
5.78
|
522.00
|
PWM-22-157
|
|
35.94
|
37.00
|
1.06
|
0.88
|
0.03
|
899.00
|
PWM-22-160
|
no significant
values
|
|
|
|
|
PWM-22-161
|
|
32.81
|
37.00
|
4.19
|
0.84
|
0.02
|
334.65
|
PWM-22-161
|
including
|
32.81
|
34.00
|
1.19
|
1.81
|
0.03
|
361.00
|
PWM-22-162
|
no significant
values
|
|
|
|
|
|
|
|
|
|
|
Drill holes are
oriented perpendicular to the strike length of the pegmatite, so
mineralization is close to true width.
|
Table 2 Assay highlights from aplite zones, West Joe Dyke,
drill holes PWM-22-148 to 162.
BHID
|
From
(m)
|
To
(m)
|
Length
(m)
|
Li2O
(%)
|
Ta
(ppm)
|
PWM-22-150
|
32.00
|
34.88
|
3.88
|
0.07
|
331.35
|
PWM-22-152
|
35.00
|
36.00
|
1.00
|
0.24
|
294.00
|
PWM-22-152
|
44.10
|
44.63
|
0.53
|
0.06
|
532.00
|
PWM-22-153
|
31.11
|
32.05
|
0.94
|
0.24
|
518.00
|
PWM-22-153
|
34.38
|
34.85
|
0.47
|
0.02
|
221.00
|
PWM-22-153
|
51.00
|
52.00
|
1.00
|
0.09
|
190.00
|
PWM-22-154
|
31.47
|
31.80
|
0.33
|
0.03
|
255.00
|
PWM-22-154
|
53.00
|
54.00
|
1.00
|
0.01
|
161.00
|
PWM-22-157
|
35.94
|
40.00
|
4.06
|
0.42
|
469.69
|
PWM-22-157
|
53.00
|
54.00
|
1.00
|
0.06
|
326.00
|
PWM-22-158
|
60.49
|
60.73
|
0.24
|
0.02
|
231.00
|
PWM-22-159
|
69.65
|
70.08
|
0.43
|
0.01
|
164.00
|
PWM-22-161
|
35.00
|
36.00
|
1.00
|
0.42
|
612.00
|
PWM-22-161
|
37.00
|
37.66
|
0.66
|
0.03
|
168.00
|
PWM-22-161
|
48.03
|
50.26
|
2.23
|
0.03
|
267.84
|
|
|
|
|
|
|
Drill holes are
oriented perpendicular to the strike length of the pegmatite, so
mineralization is close to true width.
|
This press release discloses cesium mineralization in drill holes
PWM-22-148, 149,150, 151 and 156. Pollucite is the only ore mineral
of Cs. The West Joe pollucite zone is characterized by secondary
lepidolite (Li) and muscovite along fractures in massive white
pollucite. The pollucite zone is enclosed within the inner
intermediate zone consisting of coarse-grained pale green spodumene
(Li), coarse-grained white K-feldspar enriched in Rubidium (Rb),
and Ta-oxide minerals.
In addition to the Li-Cs-Ta grades, West Joe has the advantages
that the pollucite has shallow depths of less than 50 m below surface and road access to make it
easy for future extraction. Another advantage of West Joe is that
it has three economic commodities in the same zone: lithium, cesium
and tantalum. Canadian, Ontarian and United States governments have labelled all
three commodities as critical metals.
Dr. Selway is pleased to announce high grade Li-Cs-Ta
mineralization as a result of additional drilling on the West Joe
Dyke at Case Lake as a follow up on Power Metals press releases
dated August 19 and Oct 13, 2022. Power Metals has now intersected
the pollucite zone at West Joe in 16 drill holes showing its
continuity, consistency and predictability. West Joe Dyke's easy access, shallow depth and three
commodities makes it ideal for future extraction. West Joe is
proving to be just as valuable as the Main Dyke at Case Lake.
Power Metals 2022 summer drill program is for 5,000 m and over 2,700
m has been completed to date. This press release reports
assays received to date from drill holes PWM-22-148 to 162 on the
West Joe Dyke. The purpose of each drill hole was to infill on
known mineralization to aid in a future resource estimate and to
explore to expand known mineralization.
Drill hole collar coordinates are given in Table 3.
Table 3 West Joe, Case Lake drill hole collar coordinates.
NAD 83, Zone 17. Trimble R2 GPS survey with 2 cm accuracy in the
horizontal.
Drill
Hole
|
Easting
(m)
|
Northing
(m)
|
Elevation
(m)
|
Azimuth
(◦)
|
Dip
(◦)
|
Length
(m)
|
PWM-22-148
|
576325.46
|
5431113.69
|
344.68
|
170
|
-45
|
36
|
PWM-22-149
|
576323.85
|
5431119
|
344.46
|
170
|
-45
|
42
|
PWM-22-150
|
576321.4
|
5431132.43
|
343.4
|
170
|
-45
|
51
|
PWM-22-151
|
576319.95
|
5431139.08
|
343.12
|
170
|
-45
|
52.5
|
PWM-22-152
|
576319.35
|
5431142.5
|
342.48
|
170
|
-45
|
66
|
PWM-22-153
|
576319.25
|
5431142.9
|
342.66
|
170
|
-55
|
66.5
|
PWM-22-154
|
576319.22
|
5431143.17
|
342.79
|
170
|
-65
|
81
|
PWM-22-155
|
576305.28
|
5431164.42
|
339.21
|
170
|
-45
|
86
|
PWM-22-156
|
576331.36
|
5431127.52
|
343.98
|
170
|
-45
|
48
|
PWM-22-157
|
576328.12
|
5431148.63
|
341.89
|
170
|
-45
|
81
|
PWM-22-158
|
576326.91
|
5431170.97
|
337.17
|
170
|
-45
|
90
|
PWM-22-159
|
576332.81
|
5431180.61
|
336.31
|
170
|
-45
|
136
|
PWM-22-160
|
576321.75
|
5431185.3
|
335.43
|
170
|
-70
|
161
|
PWM-22-161
|
576328.43
|
5431140.78
|
342.07
|
170
|
-45
|
60
|
PWM-22-162
|
576120
|
5431199
|
341
|
170
|
-45
|
111
|
|
|
|
|
|
|
|
Quality Control
The drill core was sampled so that 1
m of the Case Batholith tonalite host rock was sampled
followed by 1 m long samples of the
pegmatite dyke and 1 m of the Case
Batholith. The sampling followed lithology boundaries so that only
one lithology unit is within a sample, except for the < 20 cm
pegmatite veins in tonalite which were merged into one sample. The
drill core samples were delivered to SGS preparation lab in
Cochrane by Power Metals'
geologists. The core was prepared at SGS Garson and analyzed at SGS
Burnaby, British Columbia which
has ISO 17025 certification. Every 20 samples included one external
quartz blank, one external lithium standard and one core duplicate.
The ore grade Li2O% was prepared by sodium peroxide
fusion with analysis by ICP-OES with a detection limit of 0.002 %
Li2O. A Quality Control review of the standards, blanks
and core duplicates indicated that they all passed. The ore grade
Cs2O% for > 10,000 ppm Cs was prepared by alkaline
metal digestion with analysis by FAAS with a detection limit of
0.002 % Cs. Ore grade cesium was analyzed by SGS Lakefield, Ontario which also has ISO 17025
certification.
Case Lake Property
Case Lake Property is located 80 km east of Cochrane, northeastern Ontario close to the Ontario-Quebec border. Case Lake Property consists of
585 cell claims in Steele, Case, Scapa, Pliny, Abbotsford and Challies townships, Larder Lake
Mining Division. The Property is 10 km x 9.5 km in size with 14
identified tonalite domes. The Case Lake pegmatite swarm consists
of six spodumene dykes: North, Main, South, East and Northeast
Dykes on the Henry Dome and the West Joe Dyke on a new tonalite
dome. The Case Lake Property is owned 100% by Power Metals Corp. A
National Instrument 43-101 Technical Report has been prepared on
Case Lake Property and filed on July 18,
2017.
Qualified Person
Julie Selway, Ph.D., P.Geo.
supervised the preparation of the scientific and technical
disclosure in this news release. Dr. Selway is the VP of
Exploration for Power Metals and the Qualified Person ("QP") as
defined by National Instrument 43-101. Dr. Selway is supervising
the exploration program at Case Lake. Dr. Selway completed a Ph.D.
on granitic pegmatites in 1999 and worked for 3 years as a
pegmatite geoscientist for the Ontario Geological Survey. Dr.
Selway also has twenty-three scientific journal articles on
pegmatites.
About Power Metals Corp.
Power Metals Corp. is a diversified Canadian mining company with
a mandate to explore, develop and acquire high quality mining
projects. We are committed to building an arsenal of projects
in both lithium and high-growth specialty metals and minerals. We
see an unprecedented opportunity to supply the tremendous growth of
the lithium battery and clean-technology industries. Learn more at
www.powermetalscorp.com
ON BEHALF OF THE BOARD,
Johnathan More, Chairman &
CEO
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SOURCE POWER METALS CORP