Brixton Metals Corporation
(TSX-V: BBB, OTCQB:
BBBXF) (the “
Company” or
“
Brixton”) is pleased to announce final drill
results from the 2022 drill campaign at its wholly owned Langis
Project. The project is located in the Cobalt Camp of Ontario,
about 500km north from Toronto. The 2022 program started in early
November and was completed late December with 35 drill holes
totaling 7114.90m.
Highlights
- Hole LM-22-265 yielded 7.0m of
0.37% Cobalt from 120m depth
- Including 4.0m of 0.60%
Co
- Including 1.0m of 1.20% Co
- Hole LM-22-283 yielded 9.0m of 1037
g/t Silver from 165m depth
- Including 4.0m of 2043 g/t
Ag
- Including 1.0m of 7910 g/t Ag
Vice President of Exploration, Christina Anstey,
stated, “We are excited to have completed another round of highly
successful drilling at the Langis Project. Langis drilling
continues to generate impressive silver and cobalt intercepts.
While the Company currently does not have a 2023 budget for this
project, it does warrant further exploration drilling.”
Figure 1. Location of the Langis Project,
Ontario.
Table 1. Select Mineralized Intervals.
Hole |
From (m) |
To (m) |
Interval (m) |
Co (%) |
Ag (g/t) |
Ni (%) |
|
LM22-265 |
120.00 |
127.00 |
7.00 |
0.37 |
11.0 |
|
|
including |
121.00 |
125.00 |
4.00 |
0.60 |
18.3 |
|
|
including |
123.00 |
124.00 |
1.00 |
1.20 |
17.4 |
|
|
|
144.00 |
147.00 |
3.00 |
0.17 |
14.8 |
|
|
including |
145.00 |
146.00 |
1.00 |
0.46 |
14.7 |
|
|
LM22-283 |
165.00 |
174.00 |
9.00 |
0.07 |
1037 |
|
|
including |
170.00 |
174.00 |
4.00 |
0.10 |
2043 |
|
|
including |
172.00 |
173.00 |
1.00 |
0.39 |
7910 |
0.18 |
|
|
|
|
|
|
|
|
|
All assay values are uncut weighted averages and
intervals reflect drilled lengths as further drilling is required
to determine the true widths of the mineralization.
Figure 2. Collar Locations, Drill Traces and
UG-Workings Projected to Surface at the Langis Project.
Discussion
Cobalt and silver mineralization at Langis
appear to be derived from separate mineralizing events, although
the host veins commonly share structures with one another and the
two can occur together frequently. West-northwest, northwest and
east-west trends have been identified for these cobalt- and
silver-hosting structures. Cobalt mineralization appears to favor
the Coleman Member conglomerates of the Gowganda Formation,
immediately above the Keewatin mafic volcanic rocks, although
mineralized veins are observed within the mafic volcanics, as well
as within the Nipissing diabase. Cobalt occurs as cobaltite and
other Ni-Co-arsenides and sulpharsenides, hosted within
quartz-calcite veins. The veins commonly contain pyrite,
pyrrhotite, chalcopyrite, sphalerite, galena and trace native
bismuth.
Brixton has completed four previous drill
campaigns on the Langis Project, all of which have predominantly
targeted high-grade silver around the historic workings. Through
these programs, several high-grade cobalt intercepts have been
observed, including 3.5m of 1.89% Co in LM-22-254, 0.98m of 3.55%
Co in LM-18-23, and 1.0m of 1.965% Co and 20,995 g/t Ag in
LM-18-42. For this fifth season, targeting is focussed on cobalt
specific structures, testing their continuity and grade. Drill
planning involved the use of geology and geochemistry from previous
drilling, geophysical surveys and historic underground mapping
completed by Agnico in the 1980’s. Prior to 2022, Brixton had
drilled over 35,100 meters on the Langis Project. The 2022 season
started in early November and was completed late December with 35
drill holes totaling 7114.90m.
Figure 3. Collar Locations, Assays and UG
Workings Projected to Surface at the Langis Project.
Figure 4. Shaft 6 Collar Locations and Assays at
the Langis Project.
Figure 5. High-grade cobalt intercept from hole
LM-22-265.
Figure 6. Native Silver & Cobalt
Mineralization from hole LM-22-283 at 172.95m Depth.
Drill holes LM-22-260 and LM-22-265 were drilled
from the same pad location and targeted high-grade cobalt
mineralization around previously released hole LM-22-254 where 30m
averaging 0.35% cobalt was intersected. LM-22-265 was successful in
intersecting the mineralized structure and returned assays of 0.37%
cobalt over 7.0m, including 4.0m of 0.6% cobalt and 1.0m of 1.2%
cobalt (see Figure 3). Hole LM-22-260 intersected 2.0m of 0.33%
cobalt between 141.00 and 143.00m, as well as 22.50m of 0.12%
nickel between 168.0 and 190.50m.
An additional ten step-out drill holes were
completed to target the extents of the cobalt mineralization around
LM-22-265. Holes LM-22-256 and LM-22-257 were drilled 25m south
along strike of hole LM-22-254. Hole 256 intercepted 1.0m of 0.15%
cobalt between 144.50 and 145.50m, as well as 7.48m of 0.15% nickel
between 165.36 and 172.84m. LM-22-257 was drilled below hole 256
and intercepted 47.50m of 0.13% nickel and 0.01% cobalt. Holes
LM-22-258 and LM-22-259 were drilled approximately 57m north of the
previously mentioned holes and had lower grade intercepts with
assays up to 0.14% cobalt over 0.5m from hole LM-22-258. LM-22-259
intercepted broader low-grade mineralization assaying 0.01% cobalt
and 0.13% nickel over 26m from 121.0 to 147.0m as well as 5.0m of
227.4 g/t silver between 103.50 and 108.50m depth. LM-22-263 and
LM-22-264 were drilled from the same location approximately 155m
west of LM-22-258 targeting the mineralized zone from the west.
LM-22-263 intercepted 1.50m of 154.0 g/t Ag between 144.0 and
145.50m while LM-22-264 had no significant results.
LM-22-266 and LM-22-267 were drilled from the
same location approximately 40m south of LM-22-265 and intercepted
broad low-grade nickel cobalt mineralization hosted in thin
isolated veins hosted in both the Coleman Member conglomerate and
Archean mafic volcanics. LM-22-266 intercepted 26.0m of 0.12%
nickel and 0.01% cobalt while LM-22-267 intersected 10m of 0.17%
nickel and 0.06% cobalt between 134.0 and 144.0m. LM-22-268 and
LM-22-269 were drilled from the same location approximately 50m
south LM-22-266. Both holes intercepted low-grade cobalt and nickel
mineralization including 20m of 0.16% nickel and 0.01% Co,
including 8.0m of 0.20% nickel, between 166.0 and 186.00m in
LM-22-268. Hole LM-22-269 intercepted 1.0m of 0.17% cobalt between
161.0 and 162.0m and 17.26m of 0.14% nickel between 168.74 and
186.0m.
LM-22-261 and LM-22-262 were planned as step
holes to target high-grade silver mineralization previously
identified in 2021. Both holes drilled towards the northwest and
intersected approximately 80m of Coleman Member sandstone and
siltstone overlying Archean mafic volcanics. LM-22-261 intercepted
0.74m of 0.06% cobalt and 31.6 g/t Ag while LM-22-262 had no
significant results.
LM-22-270 and LM-22-271 were drilled from the
same location drilling towards the northeast and planned to test
potential mineralization between Shaft 3 to the south and Shaft 4
to the north. LM-22-270 was drilled at a dip of -42 degrees and
intersected 2.0m of 0.02% cobalt between 163.0 and 165.0m hosted in
conglomerate near the contact with Archean mafic volcanics.
LM-22-271 was steepened below LM-22-270 and intersected 0.06%
cobalt over 21.0m, including 7.50m of 0.11% cobalt, and including
3.0m of 0.2% cobalt. Additional drilling is needed around these
holes to further test the extents of the newly discovered cobalt
mineralization in this area.
LM-22-272 failed to reach depth after
intercepting historic underground mine workings. The drill was
relocated 30m north to move away from the workings and LM-22-273
and LM-22-274 were both drilled from this location. All three holes
were planned as >250m northern step-outs from the historic Shaft
6 underground workings where significant silver and cobalt
mineralization had been mined and where limited data had previously
existed. Both holes were drilled from the west and were
unsuccessful in intercepting mineralization returning no
significant assays. LM-22-275 was drilled 75m north of LM-22-274
and drilled from the east intercepting 17.32m of 0.01% cobalt.
Drill holes LM-22-276 to LM-22-281 were planned
as a series of step-out holes targeting previously identified
high-grade nickel and silver mineralization east of the Shaft 6
mine workings. All six holes were drilled towards the east,
targeting the lower contact of the diabase sill with the underlying
Archean volcanics and Coleman Member sediments, a favorable horizon
for the localization of mineralized veins. LM-22-276 and 277 were
drilled from the same location and hole 276 intercepted 16m of
0.04% cobalt, including 4.20m of 0.11% cobalt. LM-22-277 was
drilled below 276 and intercepted 5.0m of 87 g/t silver including
1.0m of 309 g/t silver between 120.0 and 125.0m. From 134.06 to
237.0m, assays returned 0.12% nickel over 102.94m, including 1.80m
of 0.33% nickel and 0.05% cobalt. LM-22-278 and 279 were drilled
from the same location 50m south of LM-22-277. LM-22-278
intersected broad anomalous nickel and cobalt but returned no
significant assay results. LM-22-279 was drilled below hole 278 and
intersected 134.0m of 0.12% nickel between 163.0 and 297.0m depth,
including 1.5m of 0.16% nickel, 0.02% cobalt and 49 g/t silver.
LM-22-280 and 281 were drilled from the same location 45m south of
LM-22-279 and achieved greater results compared to the previous
step-out holes to the north. LM-22-280 intercepted 3.0m of 0.11%
nickel and 494 g/t silver between 246.0 and 249.0m within a broader
zone of lower grade mineralization as at depth intersected 6.0m of
0.17% cobalt between 283.50 and 289.50m. LM-22-281 was drilled
below hole 280 and assayed 0.1% nickel, 0.03% Co and 424 g/t silver
over 1.50m between 174.50 and 176.0m.
LM-22-282 was drilled at an azimuth of 83
degrees with a dip of -48 degrees and was planned as a deeper hole
targeting a north-south trending conductivity anomaly. The hole
intersected diabase and Coleman Member sediments before
intercepting the anomaly where the hole transitioned into the
Archean mafic volcanics at 291.0m. The hole was drilled to a final
depth of 501.0m and assayed 0.12% nickel over 13.50m between 403.50
and 417.0m.
LM-22-283 was drilled to test an aeromagnetic
anomaly as well as the southern extension of high-grade nickel and
silver mineralization previously identified around the historic
Shaft 6 workings. The hole was drilled due east at a -45 degree dip
and intersected 100m of diabase sill above Coleman Formation
conglomerate. High-grade silver-cobalt mineralization assaying up
to 7910 g/t Ag and 0.39% Co was intercepted between 172 and 173m
depth, approximately 10m below the contact between the two units.
Drill hole LM-22-284 was drilled 80m south of LM-22-283 but no
significant assays were received. Additional follow-up drilling is
needed to determine the extents and orientations of the mineralized
structure.
Drill holes LM-22-285 to 288 were drilled
farther west on the property around the historic Shaft 3 and
planned to target cobalt mineralization previously identified by
drilling in 2021. Holes 285 and 286 were drilled from the same
location and hole 285 was cancelled after intercepting historic
mine workings and therefore no significant assays were received.
LM-22-286 intercepted 13.50m of 32.0 g/t silver including 1.5m of
227 g/t silver and was ended short to avoid mine workings. Drill
holes LM-22-287 and 288 were relocated further southwest and
achieved better results as the holes reached greater depths.
LM-22-287 had no significant assays while LM-22-288 intercepted
84.0m of 0.02% cobalt, including 1.0m of 0.11% cobalt. LM-22-288
ended in elevated cobalt due to timing constraints at the end of
the season.
Overall, the results from the 2022 drilling
campaign were successful in identifying new zones of cobalt, nickel
and silver mineralization at the Langis property and further
drilling is required to test the extents and potential of these
zones. Additionally, a total of 78 targets across 8 anomalous zones
were identified from the 2022 Alpha Induced Polarization survey
with 50 high priority targets that remain to be tested with
drilling.
Table 2. Drill Hole Assay Information.
Hole |
From (m) |
To (m) |
Interval (m) |
Co (%) |
Ag (g/t) |
Ni (%) |
|
LM22-256 |
134.00 |
146.50 |
12.50 |
0.05 |
|
|
|
including |
144.50 |
145.50 |
1.00 |
0.15 |
|
|
|
|
165.36 |
172.84 |
7.48 |
|
|
0.15 |
|
|
183.00 |
198.00 |
15.00 |
|
|
0.11 |
|
LM22-257 |
139.50 |
187.00 |
47.50 |
0.01 |
1.2 |
0.13 |
|
LM22-258 |
104.50 |
106.00 |
1.50 |
0.08 |
8.8 |
|
|
including |
105.00 |
105.50 |
0.50 |
0.14 |
4.5 |
|
|
LM22-259 |
103.50 |
108.50 |
5.00 |
|
227.4 |
|
|
|
121.00 |
147.00 |
26.00 |
0.01 |
|
0.13 |
|
LM22-260 |
141.00 |
143.00 |
2.00 |
0.33 |
|
|
|
|
168.00 |
190.50 |
22.50 |
|
|
0.12 |
|
LM22-261 |
129.10 |
129.84 |
0.74 |
0.06 |
31.6 |
|
|
LM22-262 |
No Significant Assays |
|
LM22-263 |
144.00 |
149.00 |
5.00 |
0.01 |
53.1 |
|
|
including |
144.00 |
145.50 |
1.50 |
0.01 |
154.0 |
|
|
LM22-264 |
No Significant Assays |
|
LM22-265 |
120.00 |
127.00 |
7.00 |
0.37 |
11.0 |
|
|
including |
121.00 |
125.00 |
4.00 |
0.60 |
18.3 |
|
|
including |
123.00 |
124.00 |
1.00 |
1.20 |
17.4 |
|
|
|
144.00 |
147.00 |
3.00 |
0.17 |
14.8 |
|
|
including |
145.00 |
146.00 |
1.00 |
0.46 |
14.7 |
|
|
LM22-266 |
160.00 |
186.00 |
26.00 |
0.01 |
1.4 |
0.12 |
|
LM22-267 |
134.00 |
144.00 |
10.00 |
0.06 |
1.3 |
0.17 |
|
LM22-268 |
166.00 |
186.00 |
20.00 |
0.01 |
2.8 |
0.16 |
|
including |
175.00 |
183.00 |
8.00 |
0.01 |
1.3 |
0.20 |
|
LM22-269 |
161.00 |
162.00 |
1.00 |
0.17 |
1.7 |
|
|
|
168.74 |
186.00 |
17.26 |
0.01 |
|
0.14 |
|
LM22-270 |
163.00 |
165.00 |
2.00 |
0.02 |
1.0 |
0.14 |
|
LM22-271 |
66.00 |
87.00 |
21.00 |
0.06 |
|
|
|
including |
79.50 |
87.00 |
7.50 |
0.11 |
1.0 |
|
|
including |
81.00 |
84.00 |
3.00 |
0.20 |
2.0 |
|
|
LM22-272 |
Not Assayed |
|
LM22-273 |
No Significant Assays |
|
LM22-274 |
No Significant Assays |
|
LM22-275 |
132.00 |
149.32 |
17.32 |
0.01 |
|
|
|
|
183.00 |
192.00 |
9.00 |
0.02 |
|
|
|
LM22-276 |
142.00 |
158.00 |
16.00 |
0.04 |
5.9 |
|
|
including |
145.10 |
151.87 |
6.77 |
0.07 |
8.2 |
|
|
including |
145.10 |
149.30 |
4.20 |
0.11 |
11.8 |
|
|
including |
145.10 |
145.60 |
0.50 |
0.48 |
88.7 |
0.23 |
|
LM22-277 |
120.00 |
129.04 |
9.04 |
|
50.2 |
|
|
including |
120.00 |
125.00 |
5.00 |
0.01 |
86.6 |
|
|
including |
122.00 |
123.00 |
1.00 |
|
309.0 |
|
|
|
134.06 |
237.00 |
102.94 |
0.01 |
2.3 |
0.12 |
|
including |
172.00 |
174.00 |
1.80 |
0.05 |
18.5 |
0.33 |
|
LM22-278 |
127.00 |
128.14 |
1.14 |
|
32.3 |
|
|
|
162.00 |
163.50 |
1.50 |
0.01 |
34.1 |
|
|
|
174.00 |
231.00 |
57.00 |
0.01 |
2.1 |
|
|
LM22-279 |
163.00 |
297.00 |
134.00 |
0.01 |
1.6 |
0.12 |
|
including |
187.00 |
188.50 |
1.50 |
0.02 |
49.3 |
0.16 |
|
LM22-280 |
126.00 |
303.00 |
177.00 |
0.02 |
9.7 |
|
|
including |
246.00 |
249.00 |
3.00 |
|
494.0 |
0.11 |
|
and including |
283.50 |
289.50 |
6.00 |
0.17 |
7.8 |
|
|
LM22-281 |
174.50 |
176.00 |
1.50 |
0.03 |
424.0 |
0.10 |
|
LM22-282 |
403.50 |
417.00 |
13.50 |
0.01 |
|
0.12 |
|
LM22-283 |
79.00 |
213.00 |
134.00 |
0.01 |
70.4 |
|
|
including |
165.00 |
174.00 |
9.00 |
0.07 |
1037 |
|
|
including |
170.00 |
174.00 |
4.00 |
0.10 |
2043 |
|
|
including |
172.00 |
173.00 |
1.00 |
0.39 |
7910 |
0.18 |
|
LM22-284 |
No Significant Assays |
|
LM22-285 |
No Significant Assays |
|
LM22-286 |
31.50 |
45.00 |
13.50 |
0.01 |
32.0 |
|
|
including |
43.50 |
45.00 |
1.50 |
0.01 |
227.0 |
|
|
LM22-287 |
No Significant Assays |
|
LM22-288 |
66.00 |
150.00 |
84.00 |
0.02 |
|
|
|
including |
110.00 |
111.00 |
1.00 |
0.11 |
|
|
|
Table 3. Drill Collar and Hole Information.
L A N G I S P R O J E C T D R I L L H O L E S |
Hole ID |
Easting |
Northing |
Elevation (m) |
Azimuth |
Dip |
Depth (m) |
LM-22-256 |
607178 |
5270818 |
215 |
275 |
-58 |
198.0 |
LM-22-257 |
607179 |
5270818 |
215 |
268 |
-67 |
201.0 |
LM-22-258 |
607177 |
5270875 |
215 |
261 |
-55 |
201.0 |
LM-22-259 |
607177 |
5270875 |
215 |
266 |
-63 |
200.0 |
LM-22-260 |
607021 |
5270834 |
206 |
92 |
-57 |
195.0 |
LM-22-261 |
607060 |
5270883 |
207 |
292 |
-63 |
195.0 |
LM-22-262 |
607060 |
5270883 |
207 |
293 |
-58 |
180.0 |
LM-22-263 |
607028 |
5270879 |
207 |
65 |
-44 |
210.0 |
LM-22-264 |
607027 |
5270879 |
207 |
66 |
-53 |
159.0 |
LM-22-265 |
607020 |
5270835 |
208 |
89 |
-50 |
186.0 |
LM-22-266 |
607050 |
5270796 |
209 |
97 |
-51 |
186.0 |
LM-22-267 |
607050 |
5270796 |
209 |
96 |
-57 |
174.0 |
LM-22-268 |
607055 |
5270750 |
198 |
91 |
-46 |
186.0 |
LM-22-269 |
607054 |
5270750 |
198 |
94 |
-51 |
186.0 |
LM-22-270 |
606967 |
5271021 |
193 |
62 |
-42 |
201.0 |
LM-22-271 |
606967 |
5271021 |
193 |
62 |
-48 |
180.0 |
LM-22-272 |
607282 |
5271062 |
214 |
60 |
-45 |
16.4 |
LM-22-273 |
607271 |
5271084 |
214 |
55 |
-46 |
213.0 |
LM-22-274 |
607270 |
5271082 |
214 |
74 |
-54 |
186.0 |
LM-22-275 |
607435 |
5271199 |
223 |
263 |
-43 |
201.0 |
LM-22-276 |
607455 |
5270808 |
218 |
75 |
-57 |
300.0 |
LM-22-277 |
607455 |
5270808 |
218 |
76 |
-62 |
237.0 |
LM-22-278 |
607472 |
5270762 |
217 |
80 |
-63 |
231.0 |
LM-22-279 |
607472 |
5270762 |
217 |
75 |
-53 |
297.0 |
LM-22-280 |
607509 |
5270730 |
217 |
78 |
-49 |
303.0 |
LM-22-281 |
607508 |
5270730 |
217 |
78 |
-64 |
300.0 |
LM-22-282 |
607519 |
5270692 |
218 |
83 |
-48 |
501.0 |
LM-22-283 |
607391 |
5270639 |
215 |
90 |
-45 |
219.0 |
LM-22-284 |
607420 |
5270559 |
217 |
75 |
-45 |
252.0 |
LM-22-285 |
606509 |
5270664 |
188 |
203 |
-44 |
48.0 |
LM-22-286 |
606506 |
5270665 |
188 |
213 |
-44 |
55.5 |
LM-22-287 |
606503 |
5270651 |
189 |
215 |
-42 |
162.0 |
LM-22-288 |
606531 |
5270632 |
190 |
197 |
-44 |
150.0 |
Quality Assurance & Quality
Control
Quality assurance and quality control protocols
for drill core sampling was developed by Brixton. Core samples were
mostly taken at 1.0m intervals. Blank, duplicate (lab pulp) and
certified reference materials were inserted into the sample stream
for at least every 10 drill core samples. Core samples were cut in
half, bagged, zip-tied and sent directly to ALS Minerals
preparation and analysis facility in Sudbury, Ontario. ALS Minerals
Laboratories is registered to ISO 9001:2008 and ISO 17025
accreditations for laboratory procedures. Samples were analyzed for
Ag, Co, Ni and Cu and 44 additional elements using four acid
digestion with an ICP-MS finish. The standards, certified reference
materials, were acquired from CDN Resource Laboratories Ltd., of
Langley, British Columbia and the standards inserted varied
depending on the type and abundance of mineralization visually
observed in the primary sample. Blank material used consisted of
non-mineralized siliceous landscaping rock. A copy of the QAQC
protocols can be viewed at the Company’s website.
About the Langis Project
Brixton’s wholly owned Langis Project has
excellent infrastructure and is a past producing mine located 500km
north from Toronto, Ontario, Canada. The property sits at the
northern end of Lake Temiskaming, 20km north of Electra’s Cobalt
Refinery, which should be operational in 2023. The silver
mineralization occurs as native silver and within
steeply-moderately and in some cases shallow dipping veins,
veinlets and as disseminations, rosettes and fracture infill and
can be associated with calcite, hematite, pyrite, cobaltite,
chalcopyrite, niccolite and gold. Mineralization is hosted within
any of the three main rock types: Archean Keewatin volcanic and
metasedimentary rocks, Proterozoic Coleman Member sedimentary rocks
of the Huronian Supergroup and Proterozoic Nipissing diabase. The
Langis Mine produced 10.6Moz of silver at 25 opt Ag and 358,340
pounds of cobalt from 1908 to 1989. Historically, the combined
mines in the Cobalt Camp produced over 550 million ounces of silver
with 30-50 million pounds of cobalt as a by-product.
Qualified Person
Mr. Corey A. James, P.Geo., is a Senior Project
Geologist for the Company who is a qualified person as defined by
National Instrument 43-101. Mr. James has verified the data
disclosed in this press release, including the sampling,
analytical and test data underlying the information and has
approved the technical information in this press release.
About Brixton Metals
Corporation
Brixton Metals is a Canadian exploration company
focused on the advancement of its mining projects. Brixton wholly
owns four exploration projects: Brixton’s flagship Thorn
copper-gold-silver-molybdenum Project, the Atlin Goldfields
Projects located in NW BC (under Option to Pacific Bay Minerals,
TSXV: PBM), the Langis-HudBay silver-cobalt-nickel Project in
Ontario, and the Hog Heaven copper-silver-gold Project in NW
Montana, USA (under option to Ivanhoe Electric Inc. NYSE: IE).
Brixton Metals Corporation shares trade on the TSX-V under the
ticker symbol BBB, and on the OTCQB under the
ticker symbol BBBXF. For more information about
Brixton, please visit our website at www.brixtonmetals.com.
On Behalf of the Board of Directors
Mr. Gary R. Thompson, Chairman and CEOTel:
604-630-9707 or email: info@brixtonmetals.com
For Investor Relations, please contact:
Neil MacRae, Investor RelationsTel: 604-630-9707
or email: neil.macrae@brixtonmetals.com
Neither the TSX Venture Exchange nor its
Regulation Services Provider (as that term is defined in the
policies of the TSX Venture Exchange) accepts responsibility for
the adequacy or accuracy of this release.
Information set forth in this news release may
involve forward-looking statements under applicable securities
laws. Forward-looking statements are statements that relate to
future, not past, events. In this context, forward-looking
statements often address expected future business and financial
performance, and often contain words such as “anticipate”,
“believe”, “plan”, “estimate”, “expect”, and “intend”, statements
that an action or event “may”, “might”, “could”, “should”, or
“will” be taken or occur, including statements that address
potential quantity and/or grade of minerals, potential size and
expansion of a mineralized zone, proposed timing of exploration and
development plans, or other similar expressions. All statements,
other than statements of historical fact included herein including,
without limitation, statements regarding the use of proceeds. By
their nature, forward-looking statements involve known and unknown
risks, uncertainties and other factors which may cause our actual
results, performance or achievements, or other future events, to be
materially different from any future results, performance or
achievements expressed or implied by such forward-looking
statements. Such factors include, among others, the following
risks: the need for additional financing; operational risks
associated with mineral exploration; fluctuations in commodity
prices; title matters; and the additional risks identified in the
annual information form of the Company or other reports and filings
with the TSXV and applicable Canadian securities regulators.
Forward-looking statements are made based on management’s beliefs,
estimates and opinions on the date that statements are made and the
Company undertakes no obligation to update forward-looking
statements if these beliefs, estimates and opinions or other
circumstances should change, except as required by applicable
securities laws. Investors are cautioned against attributing undue
certainty to forward-looking statements.
Photos accompanying this announcement are
available at
https://www.globenewswire.com/NewsRoom/AttachmentNg/7f3406e6-d8c4-4a05-a92f-5579fd79e8c8
https://www.globenewswire.com/NewsRoom/AttachmentNg/e1e9d1a2-3580-4bd9-8904-30291ec3ddc7
https://www.globenewswire.com/NewsRoom/AttachmentNg/0785377a-f509-4a7d-870c-3ab88e1eae89
https://www.globenewswire.com/NewsRoom/AttachmentNg/c5e4157c-b0f0-48a8-bf6e-a16203362d03
https://www.globenewswire.com/NewsRoom/AttachmentNg/e75a601f-193c-44d2-805e-c1633f4c06a0
https://www.globenewswire.com/NewsRoom/AttachmentNg/dd826f4a-34d1-4313-8e05-af9ed3098796
Pacific Bay Minerals (TSXV:PBM)
과거 데이터 주식 차트
부터 11월(11) 2024 으로 12월(12) 2024
Pacific Bay Minerals (TSXV:PBM)
과거 데이터 주식 차트
부터 12월(12) 2023 으로 12월(12) 2024