Fission Regional Exploration Drilling at Saloon East Hits Strongest Radioactivity to Date Outside of the Triple R Deposit
ir@fissionuranium.com
www.fissionuranium.com
TSX SYMBOL: FCU
OTCQX SYMBOL:
FCUUF
>90% of holes on
Drilling Highlights
- Summer regional exploration drilling tested ~8.8km of the
Saloon Shear Zone with 14 holes, with >90% of the holes intersecting anomalous radioactivity in multiple intervals in each hole. These results represent the strongest hydrothermal alteration and radioactivity encountered to date at PLS outside of theTriple R deposit. - Drilling along the
Saloon Shear Zone intersected anomalous radioactivity along 8km of strike length with most prospective results at Saloon Main and East areas. - Saloon Main – tested by 5 holes and all encountering anomalous radioactivity associated with strong hydrothermal alteration.
-
- Hole PLS24-679A intersected a total composite of 65.5m of anomalous radioactivity with peaks up to 4,077 cps.
- Hole PLS24-661 intersected a total composite of 137.4m anomalous radioactivity over a 394.6m interval, with peaks up to 3,254.1 cps, suggesting the Saloon Main shear zone remains prospective to a depth of at least 540m below surface.
- Saloon East – Tested by 3 holes and all encountering anomalous radioactivity associated with strong hydrothermal alteration.
-
- Hole PLS24-684B intersected five intervals of anomalous radioactivity over considerable widths, with the strongest results from an 11.6m wide interval with a peak of 12,677.6 cps and a 4m wide interval with peak of 6,737.7 cps.
- Hole PLS24-680 intersected eight intervals of anomalous radioactivity over a total composite width of 25.9m, with the strongest results from a 6.8m wide interval with a peak 10,428.7 cps and a 1.1m wide interval with a peak of 7,833.6 cps.
- Hole PLS24-682 encountered six intervals of anomalous radioactivity with the best results from a 5.1m wide interval returning a peak of 5,841.8 cps.
Table 1: S2024 Regional Exploration Drill Hole Summary
TARGET AREA |
Collar |
Basement Unconformity |
Total |
Downhole Gamma Probe Results (>500 cps / >0.3 m minimum) |
||||||||
HOLE ID |
Easting (UTM |
Northing (UTM |
Elevation (masl) |
Az |
Dip |
From (m) |
To |
Width (m) |
CPS Peak |
|||
Saloon Main |
PLS24-654 |
595592 |
6385529 |
550 |
313 |
-56 |
152.0 |
502.3 |
406.2 |
406.5 |
0.3 |
706.3 - 1,118.0 |
|
|
|
|
|
|
|
|
|
410.6 |
412.7 |
2.1 |
<500 - 2,084.0 |
|
PLS24-657A |
595747 |
6385697 |
552 |
313 |
-57 |
140.0 |
464.0 |
367.9 |
369.4 |
1.5 |
<500 - 694.7 |
|
|
|
|
|
|
|
|
|
370.4 |
371.2 |
0.8 |
<500 - 711.0 |
|
|
|
|
|
|
|
|
|
451.5 |
452.8 |
1.3 |
574.0 - 1,016.0 |
|
PLS24-661 |
595355 |
6385682 |
548 |
142 |
-86 |
115.8 |
768.2 |
145.9 |
146.4 |
0.5 |
511.3 - 947.1 |
|
|
|
|
|
|
|
|
|
157.8 |
176.0 |
18.2 |
<500 - 2,344.7 |
|
|
|
|
|
|
|
|
|
182.6 |
209.6 |
27.0 |
<500 - 3,254.1 |
|
|
|
|
|
|
|
|
|
259.2 |
259.7 |
0.5 |
554.1 - 702.4 |
|
|
|
|
|
|
|
|
|
261.5 |
262.0 |
0.5 |
508.2 - 729.4 |
|
|
|
|
|
|
|
|
|
265.1 |
265.6 |
0.5 |
534.1 - 975.0 |
|
|
|
|
|
|
|
|
|
269.1 |
285.2 |
16.1 |
<500 - 1,656.3 |
|
|
|
|
|
|
|
|
|
295.4 |
306.5 |
11.1 |
<500 - 2,175.3 |
|
|
|
|
|
|
|
|
|
314.2 |
328.2 |
14.0 |
<500 - 2,500.0 |
|
|
|
|
|
|
|
|
|
331.2 |
336.8 |
5.6 |
<500 - 1,248.2 |
|
|
|
|
|
|
|
|
|
342.8 |
343.1 |
0.3 |
591.1 - 851.1 |
|
|
|
|
|
|
|
|
|
346.7 |
370.9 |
24.2 |
<500 - 1,843.5 |
|
|
|
|
|
|
|
|
|
378.6 |
379.1 |
0.5 |
583.8 - 857.5 |
|
|
|
|
|
|
|
|
|
402.9 |
403.3 |
0.4 |
515.3 - 582.4 |
|
|
|
|
|
|
|
|
|
440.9 |
443.2 |
2.3 |
<500 - 2,441.3 |
|
|
|
|
|
|
|
|
|
486.1 |
486.5 |
0.4 |
592.9 - 695.3 |
|
|
|
|
|
|
|
|
|
490.7 |
494.7 |
4.0 |
<500 - 1,168.2 |
|
|
|
|
|
|
|
|
|
497.2 |
498.9 |
1.7 |
<500 - 1,341.2 |
|
|
|
|
|
|
|
|
|
508.0 |
511.0 |
3.0 |
<500 - 748.8 |
|
|
|
|
|
|
|
|
|
515.3 |
516.6 |
1.3 |
<500 - 777.6 |
|
|
|
|
|
|
|
|
|
521.5 |
523.1 |
1.6 |
<500 - 1,176.3 |
|
|
|
|
|
|
|
|
|
525.1 |
527.6 |
2.5 |
<500 - 1,404.8 |
|
|
|
|
|
|
|
|
|
539.4 |
540.5 |
1.1 |
<500 - 658.8 |
|
PLS24-679A |
595381 |
6385720 |
548 |
156 |
-80 |
125.0 |
380.0 |
205.7 |
216.9 |
11.2 |
<500 - 4,077.3 |
|
|
|
|
|
|
|
|
|
236.9 |
243.9 |
7.0 |
<500 - 2,572.0 |
|
|
|
|
|
|
|
|
|
246.5 |
253.1 |
6.6 |
<500 - 1,221.9 |
|
|
|
|
|
|
|
|
|
258.9 |
264.2 |
5.3 |
<500 - 2,655.2 |
|
|
|
|
|
|
|
|
|
272.5 |
277.3 |
4.8 |
<500 - 1,241.9 |
|
|
|
|
|
|
|
|
|
285.4 |
296.9 |
11.5 |
<500 - 1,916.2 |
|
|
|
|
|
|
|
|
|
313.8 |
315.6 |
1.8 |
524.8 - 845.7 |
|
|
|
|
|
|
|
|
|
323.5 |
337.9 |
14.4 |
<500 - 1,601.9 |
|
|
|
|
|
|
|
|
|
341.6 |
343.6 |
2.0 |
<500 - 1050.0 |
|
|
|
|
|
|
|
|
|
350.2 |
351.1 |
0.9 |
531.8 - 3,402.7 |
|
PLS24-681 |
595321 |
6385676 |
548 |
141 |
-82 |
114.4 |
332.0 |
195.4 |
196.0 |
0.6 |
<500 - 750.9 |
|
|
|
|
|
|
|
|
|
226.9 |
227.4 |
0.5 |
503.8 - 872.4 |
|
|
|
|
|
|
|
|
|
292.1 |
292.4 |
0.3 |
774.3 - 1,098.1 |
|
|
|
|
|
|
|
|
|
296.3 |
302.1 |
5.8 |
<500 - 2,830.5 |
|
|
|
|
|
|
|
|
|
320.7 |
321.2 |
0.5 |
508.2 - 700.0 |
Saloon East |
PLS24-680 |
601969 |
6388620 |
510 |
310 |
-59 |
107.3 |
410.0 |
269.4 |
274.4 |
5.0 |
<500 - 1,670.0 |
|
|
|
|
|
|
|
|
|
277.8 |
282.3 |
4.5 |
520 - 3,349.5 |
|
|
|
|
|
|
|
|
|
284.7 |
292.0 |
7.3 |
<500 - 3,990.0 |
|
|
|
|
|
|
|
|
|
300.6 |
300.9 |
0.3 |
<500 - 577.3 |
|
|
|
|
|
|
|
|
|
305.1 |
305.6 |
0.5 |
600.0 - 1,806.7 |
|
|
|
|
|
|
|
|
|
306.7 |
313.5 |
6.8 |
<500 - 10,428.7 |
|
|
|
|
|
|
|
|
|
325.3 |
326.4 |
1.1 |
723.8 - 7,833.6 |
|
|
|
|
|
|
|
|
|
360.0 |
360.4 |
0.4 |
527.6 - 624.8 |
|
PLS24-682 |
601968 |
6388620 |
510 |
310 |
-55 |
47.0 |
344.0 |
253.2 |
254.0 |
0.8 |
551.4 - 902.0 |
|
|
|
|
|
|
|
|
|
265.1 |
265.7 |
0.6 |
580.0 - 988.6 |
|
|
|
|
|
|
|
|
|
267.7 |
273.3 |
5.6 |
<500 - 1,950.5 |
|
|
|
|
|
|
|
|
|
277.4 |
277.7 |
0.3 |
590.9 - 700.0 |
|
|
|
|
|
|
|
|
|
296.1 |
301.2 |
5.1 |
<500 - 5,841.8 |
|
|
|
|
|
|
|
|
|
303.2 |
303.5 |
0.3 |
<500 - 519.1 |
|
PLS24-684B |
601969 |
6388619 |
510 |
306 |
-63 |
20.0 |
401.0 |
141.4 |
141.7 |
0.3 |
<500 - 752.6 |
|
|
|
|
|
|
|
|
|
278.0 |
289.6 |
11.6 |
<500 - 12,677.6 |
|
|
|
|
|
|
|
|
|
296.2 |
297.7 |
1.5 |
517.8 - 935.8 |
|
|
|
|
|
|
|
|
|
309.8 |
311.9 |
2.1 |
<500 - 1,022.1 |
|
|
|
|
|
|
|
|
|
315.4 |
319.4 |
4.0 |
<500 - 6,736.7 |
Saloon |
PLS24-651 |
595010 |
6384707 |
543 |
317 |
-70 |
122.5 |
458.0 |
369.1 |
369.4 |
0.3 |
530.0 - 591.7 |
|
|
|
|
|
|
|
|
|
442.0 |
442.3 |
0.3 |
<500 - 745.6 |
|
PLS24-667 |
594695 |
6383617 |
550 |
319 |
-63 |
130.6 |
389.0 |
No anomalous radioactivity |
|||
|
PLS24-670 |
598520 |
6385949 |
538 |
350 |
-57 |
110.6 |
364.0 |
223.4 |
224.4 |
1.0 |
<500 - 1,059.0 |
|
|
|
|
|
|
|
|
|
226.9 |
227.2 |
0.3 |
<500 - 676.0 |
|
|
|
|
|
|
|
|
|
245.8 |
246.4 |
0.6 |
868.6 - 2,668.0 |
|
|
|
|
|
|
|
|
|
249.5 |
249.8 |
0.3 |
<500 - 761.9 |
|
PLS24-672 |
598491 |
6386034 |
552 |
336 |
-75 |
115.3 |
252.7 |
147.7 |
148.0 |
0.3 |
<500 - 589.1 |
|
|
|
|
|
|
|
|
|
148.8 |
149.9 |
1.1 |
525.7 - 625.0 |
|
|
|
|
|
|
|
|
|
185.1 |
189.8 |
4.7 |
<500 - 2,860.9 |
|
PLS24-674 |
598441 |
6386221 |
555 |
326 |
-69 |
97.8 |
486.6 |
297.7 |
298.1 |
0.4 |
561.0 - 725.7 |
|
|
|
|
|
|
|
|
|
357.3 |
357.6 |
0.3 |
<500 - 663.0 |
|
|
|
|
|
|
|
|
|
409.4 |
410.1 |
0.7 |
750.5 - 1,461.9 |
|
|
|
|
|
|
|
|
|
425.1 |
425.6 |
0.5 |
530.0 - 1,522.7 |
|
|
|
|
|
|
|
|
|
447.3 |
447.6 |
0.3 |
<500 - 587.0 |
|
PLS24-678 |
600423 |
6386943 |
558 |
316 |
-74 |
115.6 |
506.0 |
173.3 |
173.9 |
0.6 |
530.0 - 589.3 |
|
|
|
|
|
|
|
|
|
232.3 |
232.5 |
0.3 |
<500 - 585.3 |
Far West |
PLS24-683 |
592865 |
6387008 |
550 |
309 |
-72 |
98.0 |
371.0 |
No anomalous radioactivity |
Saloon Main –
The area is located ~5km to the southwest of the
Saloon East –
The area is located ~4km to the southeast of the
Far West
The Far West target area is located ~4km west of the R1515W, along trend of the
Technical Summary for All Holes
Saloon Main
PLS24-654 was drilled 100m northeast of the main Saloon target, along the same EM trend that hosts anomalous uranium concentrations at Saloon. The drillhole intersected bedrock at a depth of 152.0m, consisting of an interfingered mafic, intermediate orthogneiss and quartz-feldspar-biotite-garnet gneiss upper zone. A thick graphitic fault zone was intersected from 243.7m to 261.8m, which is a previously untested graphitic fault zone at Saloon. This graphitic fault zone was underlain by a variably silicified sequence of orthogneiss, quartz-feldspar-biotite-garnet gneiss and sheared granitoids to 408.4m. A second graphitic fault zone was encountered at this depth, which continued to 424.3m, underlain by quartz-feldspar gneiss and intermediate orthogneiss to a final depth of 502.3m. The lower graphitic fault zone is associated with two intervals of anomalous radioactivity, from 406.2m to 406.5m and 410.0m to 412.7m with maximums of 1,118 cps and 2,084 cps, respectively.
PLS24-657A was drilled 300m northeast of the main Saloon target and tested the southern graphitic fault zone intersected in PLS24-654 along trend. Bedrock was intersected at a depth of 140.0m and consisted primarily of variably silicified quartz-feldspar-biotite-garnet gneiss, intermediate orthogneiss and mafic gneiss. Two intervals of graphitic mylonite were intersected, from 194.0m to 203.7m and 244.4m to 250.4m, which likely represent the extension of the southern graphitic fault zone seen in PLS24-654. The drillhole as terminated at a final depth of 464.0m in a thick sequence of variably silicified quartz-feldspar-biotite-garnet gneiss. Three zones of anomalous radioactivity were identified on the downhole gamma probe, from 367.9m to 369.4m, 370.4m to 371.2m and 451.5m to 452.8m, with maximums of 694.7, 711.0 and 1,016 cps, respectively.
PLS24-661 was drilled directly at the main Saloon target and was planned to drill parallel, down-dip, of the main fault zone hosting anomalous uranium concentrations at Saloon. Bedrock was intersected at 115.8m and consisted of intensely hematite and clay altered, variably silicified breccias and mafic gneisses to 490.7m, followed by an interfingered sequence of coarse garnet quartz-feldspar-biotite gneiss, sheared granitoid and pegmatites to the end of the hole at 768.2 m. A total of 137.4m of total composite radioactivity was detected on the downhole gamma probe in 23 separate zones over a 394.6m long core interval between 145.9m and 540.5m. The strongest intersections occurred between 157.8m to 176.0m and 182.6m to 209.6m with maximums of 2,344.7 and 3,254.1 cps, respectively.
PLS24-679A was drilled at the main Saloon target area, targeting the strongest radioactivity intersected in PLS24-661 30m along strike to the northeast. Bedrock was reached at a depth of 125.0m downhole and consisted of alternating extremely silicified to clay-hematite breccia to mylonitic rocks throughout the drillholes entire length to a final depth of 380.0m. A total of 65.5m of anomalous radioactivity was detected on the downhole gamma probe, with the best intervals occurring between 205.7m to 216.9m, 285.4m to 296.9m and 323.5m to 337.9m with peaks of 4,077.3 cps, 1,916.2 cps and 1,601.9 cps, respectively.
PLS24-681 was drilled at the main Saloon target area, testing the strongest radioactivity intersected in PLS24-661 30m along strike to the southwest. Bedrock was intersected at a depth of 114.4m and like other drillholes in the Saloon area, consisted of alternating very strongly silicified, hematite-clay altered, brecciated to mylonitic rocks to the end of the drillhole at 332.0m. Five zones of anomalous radioactivity were intersected, with the best occurring from 296.3m to 302.1m with a peak of 2,830.5 cps.
Saloon East
PLS24-680 tested a strong EM conductor along the South Patteson trend. It is interpreted that the top 80m of bedrock in this drillhole, consisting of Cretaceous mudstone and altered bedrock were washed away during drilling, and solid basement was intersected at a depth of 107.3m. Basement units consisted of an upper sequence of variably chlorite-clay altered intermediate orthogneiss and quartz-feldspar-biotite-garnet gneiss with wet-rock style alteration, followed by graphitic cataclasite and an intensely silicified unit. The silicified "hanging wall" was underlain by a clay altered graphitic fault zone and then mafic gneiss, sheared granitoid and quartz-feldspar-biotite-garnet gneiss to the end of the hole at 410.0m. Eight zones of elevated radioactivity totaling 25.9m were intersected between 269.4m and 360.4m. Strong radioactivity was detected from 306.7m to 313.5m hosted in the clay altered graphitic fault zone with a maximum of 10,428.7 cps, and from 325.3m to 326.4m hosted in a hematite-clay altered shear zone with a maximum of 7,833.6 cps.
PLS24-682 was drilled to test 25m up-dip of the strong radioactivity intersected in PLS24-680. Bedrock was encountered at 47.0m downhole and consisted of Cretaceous mudstone to 89.0m, followed by a similar hanging wall sequence of chlorite-clay altered intermediate orthogneiss and quartz-feldspar-biotite-garnet gneiss with wet-rock style alteration, graphitic cataclasite and a strongly silicified "hanging-wall". The silicified hanging wall was underlain by a clay altered graphitic fault zone and then sheared granitoid, mafic granofels and quartz-feldspar-biotite-garnet gneiss to the end of the hole at 344.0m. Six zones of anomalous radioactivity were encountered, with the best occurring from 267.7m to 273.3m and 296.1m to 301.2m returning peaks of 1,950.5 cps and 5,841.8 cps, respectively.
PLS24-684B was drilled to test 25m down-dip of the strong radioactivity intersected in PLS24-680. Bedrock was encountered at 20.0m downhole and consisted of Cretaceous mudstone to 68.0m, followed by a hanging wall sequence of chlorite-clay altered intermediate orthogneisses and quartz-feldspar-biotite-garnet gneiss with wet-rock style alteration, graphitic cataclasite and a strongly silicified zone. The silicified zone was underlain by a thin clay altered graphitic fault zone and then primarily quartz-feldspar-biotite-garnet gneiss to the end of the hole at 401.0m. Five zones of anomalous radioactivity were encountered, with the best occurring from 278.0m to 289.6m and 315.4m to 319.4m returning peaks of 12,677.6 cps and 6,736.7 cps, respectively.
Saloon - General
PLS24-651 was drilled 1 km southwest of the main Saloon target area, testing an airborne EM conductivity high coincident with a magnetic low running along the southern flank of a broad magnetic high. The drillhole intersected bedrock at a depth of 122.5m downhole, consisting of an upper sequence of mafic and quartz-feldspar gneisses to 214.0 m, a variably silicified and graphitic zone to 325.3m and quartz-feldspar gneisses to the end of the hole at 458.0m. Two 0.3m zones of anomalous radioactivity were detected on a 2PGA-1000 gamma probe, with maximums of 591.7 counts per second (cps) and 745.6 cps at 369.1m and 442.0m, respectively.
PLS24-667 tested a northeast trending EM conductor located south of the main Saloon target, within a broad magnetic low. Bedrock was intersected at a depth of 130.6m and consisted of an upper package of coarse garnet quartz-feldspar-biotite gneiss and intermediate orthogneiss to 223.2m, followed by variably graphite altered and structurally deformed mafic gneiss, intermediate orthogneiss and mylonite to the end of the hole at 389.0m. No anomalous radioactivity >500 cps was detected on the downhole gamma probe.
PLS24-670 tested northeast of the main Saloon target area, along a strong EM conductor coincident with a magnetic low. A 1.4m thick lens of Cretaceous mudstone was intersected at 110.6m downhole and basement units consisted primarily of intermediate orthogneiss and mafic gneiss to the final depth at 364.0m. Two broad fault zones with moderate to strong clay and graphite alteration were intersected between 194.1m to 223.4m and 251.4m to 275.0m. Four thin zones of anomalous radioactivity were detected on the downhole gamma probe associated with the graphitic damage zones, with a peak of up to 2,668 cps between 245.8m and 246.4 m.
PLS24-672 tested the clay altered, graphitic fault zones intersected in PLS24-670 up-dip near the top of bedrock. Bedrock was intersected at a depth of 115.3 m downhole and consisted primarily of variably altered intermediate orthogneiss and mafic gneiss to the final depth at 252.7 m. Strong graphite-clay alteration was intersected in a fault zone between 191.0 and 227.8 m. Three zones of anomalous radioactivity were detected on the gamma probe, including a continuous 4.7 m thick interval between 185.1 and 189.8 m with a peak of 2,860.9 cps.
PLS24-674 was drilled 290m north of PLS24-670 and 672 testing a parallel northeast trending EM conductor system, termed the South Patterson trend. A 15.2m thick lens of Cretaceous mudstone was intersected starting at 97.8m, followed by a complex, interfingered sequence of variably chloritic, silicified quartz-feldspar-biotite-garnet gneiss, intermediate orthogneiss and mafic gneiss cut by numerous strongly graphitic shear zones to a final depth of 486.6m. Interpreted dravite breccia, occurring as cm veins to 10's of cm thick breccia was intersected throughout the drillhole. Five thin zones of anomalous radioactivity were intersected with peaks up to 1,522.7 cps between 425.1m and 425.6m.
PLS24-678 tested the same trend as PLS24-670 and 672, 2 km to the northeast. Bedrock was intersected at a depth of 115.6m and consisted of an interfingered sequence of weakly to moderately chlorite altered intermediate orthogneiss, quartz-feldspar-biotite-garnet gneiss, granitoid and mafic gneiss to the end of hole depth at 506.0m. Numerous zones of graphite alteration or graphitic fault zones were intersected throughout the length of the drillhole. Two thin zones of radioactivity were detected, between 173.3m to 173.9m and 232.3m to 232.5m, with peaks of 689.3 and 585.3 cps, respectively.
Far West
PLS24-683 was drilled at the Far West target area and represents the furthest west exploration drilling the Company has performed along the PLG-3B main trend which also hosts the
Natural gamma radiation that is reported in this news release was measured in counts per second (cps) using a
All intersections are down-hole depths. All depths reported of core interval measurements including radioactivity and mineralization intervals widths are not always representative of true thickness.
Samples from the drill core will be split in half sections on site and where possible, samples will be standardized at 0.5m down-hole intervals. One-half of the split sample will be sent to
PLS Mineralized Trend & Triple R Deposit Summary
Uranium mineralization of the
The R1515W, R840W and R00E zones make up the western region of the
Mineralization along the Patterson Lake Corridor trend remains prospective along strike in both the western and eastern directions. Basement rocks within the mineralized trend are identified primarily as mafic intrusive rocks with varying degrees of alteration. Mineralization is both located within and associated with mafic intrusives with varying degrees of silicification, metasomatic mineral assemblages and hydrothermal graphite. The graphitic sequences are associated with the PL-3B basement Electro-Magnetic (EM) conductor.
Patterson Lake South Property
The 31,039-hectare PLS project is 100% owned and operated by
Qualified Persons
The technical information in this news release has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and reviewed on behalf of the company by
About
ON BEHALF OF THE BOARD
"Ross McElroy"
Cautionary Statement:
Certain information contained in this press release constitutes "forward-looking information", within the meaning of Canadian legislation. Generally, these forward-looking statements can be identified by the use of forward-looking terminology such as "plans", "expects" or "does not expect", "is expected", "budget", "scheduled", "estimates", "forecasts", "intends", "anticipates" or "does not anticipate", or "believes", or variations of such words and phrases or state that certain actions, events or results "may", "could", "would", "might" or "will be taken", "occur", "be achieved" or "has the potential to". Forward looking statements contained in this press release may include statements regarding the future operating or financial performance of the Company which involve known and unknown risks and uncertainties which may not prove to be accurate. Actual results and outcomes may differ materially from what is expressed or forecasted in these forward-looking statements. Such statements are qualified in their entirety by the inherent risks and uncertainties surrounding future expectations. Among those factors which could cause actual results to differ materially are the following: market conditions and other risk factors listed from time to time in our reports filed with Canadian securities regulators on SEDAR+ at www.sedarplus.ca. The forward-looking statements included in this press release are made as of the date of this press release and the Company disclaims any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or otherwise, except as expressly required by applicable securities legislation.
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