Strong assay results for PFS resource drilling
KELOWNA, British Columbia, Sept. 25, 2018 (GLOBE NEWSWIRE) -- FISSION URANIUM CORP.
("Fission" or “the Company") is pleased to announce assay results from nine holes drilled during
its summer 2018 program at its’ PLS property in Canada's Athabasca Basin region. All nine holes, which were targeting potential
growth and resource-upgrade areas of the Triple R deposit’s R780E zone, returned substantial high-grade intervals. Of particular
note is hole PLS18-588 (line 645E) which intersected 76.5m of total composite mineralization, including intervals
such as 15.5m @ 23.89% U3O8 in 50.5m @ 8.21% U3O8.
The goal of the summer 2018 program was to drill key areas of the R780E zone high-grade that are presently
classified as “inferred” and convert them to “indicated”. To that extent, the 9 drill holes intersected width and strength of
mineralization where expected and, in some cases, results were greater than expected. The results of the summer 2018 drill program
will be included in a new resource estimate that will be used for the upcoming pre-feasibility (“PFS”) study. The Company expects
to release the PFS study in Q4, 2018.
Assay Highlights Include:
PLS18-588 (line 645E): key intervals
-
50.5m @ 8.21% U3O8 (115.5m to 166.0m), including:
- 15.5m @ 23.89% U3O8 (142.5m to 158.0m)
PLS18-584 (line 825E): key intervals
-
42.0m @ 5.66% U3O8 (107.0m to 149.0m), including:
- 9.5m @ 18.72% U3O8 (127.5m to 137.0m), and
- 1.0m @ 8.44% U3O8 (140.5m to 141.5m)
PLS18-586 (line 525E): key intervals
-
28.7m @ 6.34% U3O8 (85.8m to 114.5m), including:
- 2.0m @ 9.29% U3O8 (95.5m to 97.5m), and
- 5.5m @ 26.03% U3O8 (108.0m to 113.5m)
-
17.0m @ 0.79% U3O8 (117.0m to 134.0m), including:
- 4.0m @ 2.46% U3O8 (127.5m to 131.5m)
Ross McElroy, President, COO, and Chief Geologist for Fission, commented,
“These final assays from summer drilling on the R780E zone include a number of very robust intercepts and
have the potential to increase the indicated category of a revised resource estimate that will be used for the resource model in
our upcoming pre-feasibility study. The width and grades we have encountered this summer are a reminder of the high quality of
mineralization contained within the Triple R deposit, which remains open in multiple directions.”
Table 1: R780E Zone - Composited Mineralized Intervals from Drill Holes
|
Zone |
Hole ID |
Grid Line |
Az |
Dip |
From (m) |
To (m) |
Interval (m) |
U3O8 (wt%) |
|
R780E |
PLS18-583 |
840E |
157 |
-69.0 |
84.00 |
88.50 |
4.50 |
0.07 |
|
|
|
|
|
|
102.00 |
103.50 |
1.50 |
0.12 |
|
|
|
|
|
|
113.00 |
146.50 |
33.50 |
4.66 |
|
|
|
|
|
|
130.50 |
139.50 |
9.00 |
15.51 |
|
|
|
|
|
|
150.00 |
154.00 |
4.00 |
0.20 |
|
|
|
|
|
|
168.50 |
169.00 |
0.50 |
0.07 |
|
|
|
|
|
|
170.00 |
170.50 |
0.50 |
0.06 |
|
|
|
|
|
|
173.50 |
180.00 |
6.50 |
0.50 |
|
|
|
|
|
|
183.00 |
184.50 |
1.50 |
0.07 |
|
|
|
|
|
|
196.00 |
197.00 |
1.00 |
0.06 |
|
|
|
|
|
|
199.50 |
200.00 |
0.50 |
0.06 |
|
|
|
|
|
|
219.00 |
225.00 |
6.00 |
0.16 |
|
|
|
|
|
|
246.50 |
263.00 |
16.50 |
0.12 |
|
|
|
|
|
|
267.00 |
270.50 |
3.50 |
0.24 |
|
|
|
|
|
|
273.50 |
281.00 |
7.50 |
0.09 |
|
|
|
|
|
|
284.50 |
285.00 |
0.50 |
0.12 |
|
|
|
|
|
|
287.00 |
287.50 |
0.50 |
0.15 |
|
|
|
|
|
|
290.50 |
299.50 |
9.00 |
0.07 |
|
|
PLS18-584 |
825E |
156 |
-69.7 |
73.50 |
74.00 |
0.50 |
0.18 |
|
|
|
|
|
|
77.00 |
81.00 |
4.00 |
0.16 |
|
|
|
|
|
|
107.00 |
149.00 |
42.00 |
5.66 |
|
|
|
|
|
|
127.50 |
137.00 |
9.50 |
18.72 |
|
|
|
|
|
|
140.50 |
141.50 |
1.00 |
8.44 |
|
|
|
|
|
|
154.50 |
162.00 |
7.50 |
0.08 |
|
|
|
|
|
|
165.50 |
166.00 |
0.50 |
0.10 |
|
|
|
|
|
|
168.50 |
171.50 |
3.00 |
0.18 |
|
|
|
|
|
|
174.00 |
177.50 |
3.50 |
0.20 |
|
|
|
|
|
|
182.00 |
184.00 |
2.00 |
0.11 |
|
|
|
|
|
|
187.00 |
195.50 |
8.50 |
0.06 |
|
|
|
|
|
|
198.00 |
204.00 |
6.00 |
0.08 |
|
|
|
|
|
|
216.00 |
218.00 |
2.00 |
0.07 |
|
|
|
|
|
|
239.00 |
239.50 |
0.50 |
0.06 |
|
|
|
|
|
|
244.00 |
246.50 |
2.50 |
0.09 |
|
|
|
|
|
|
264.00 |
272.00 |
8.00 |
0.19 |
|
|
|
|
|
|
274.50 |
285.00 |
10.50 |
0.15 |
|
|
|
|
|
|
288.50 |
289.00 |
0.50 |
0.18 |
|
|
|
|
|
|
300.50 |
302.00 |
1.50 |
0.10 |
|
|
|
|
|
|
305.00 |
305.50 |
0.50 |
0.09 |
|
|
PLS18-585 |
555E |
333 |
-69.5 |
123.00 |
123.50 |
0.50 |
0.07 |
|
|
|
|
|
|
126.00 |
128.00 |
2.00 |
0.07 |
|
|
|
|
|
|
131.00 |
158.00 |
27.00 |
3.08 |
|
|
|
|
|
|
148.50 |
155.00 |
6.50 |
9.40 |
|
|
|
|
|
|
161.00 |
161.50 |
0.50 |
0.18 |
|
|
|
|
|
|
167.50 |
174.50 |
7.00 |
0.35 |
|
|
|
|
|
|
194.00 |
201.00 |
7.00 |
0.19 |
|
|
|
|
|
|
204.00 |
209.00 |
5.00 |
0.43 |
|
|
|
|
|
|
214.50 |
215.50 |
1.00 |
0.29 |
|
|
|
|
|
|
219.50 |
221.50 |
2.00 |
0.38 |
|
|
|
|
|
|
227.50 |
236.00 |
8.50 |
0.14 |
|
|
|
|
|
|
240.00 |
245.00 |
5.00 |
0.06 |
|
|
|
|
|
|
249.00 |
256.00 |
7.00 |
0.07 |
|
|
|
|
|
|
289.00 |
289.50 |
0.50 |
0.06 |
|
|
PLS18-586 |
525E |
157 |
-69.7 |
85.80 |
114.50 |
28.70 |
6.34 |
|
|
|
|
|
|
95.50 |
97.50 |
2.00 |
9.29 |
|
|
|
|
|
|
108.00 |
113.50 |
5.50 |
26.03 |
|
|
|
|
|
|
117.00 |
134.00 |
17.00 |
0.79 |
|
|
|
|
|
|
127.50 |
131.50 |
4.00 |
2.46 |
|
|
PLS18-587 |
495E |
154 |
-69.8 |
79.50 |
96.00 |
16.50 |
0.92 |
|
|
|
|
|
|
87.00 |
91.00 |
4.00 |
2.50 |
|
|
|
|
|
|
98.50 |
102.00 |
3.50 |
0.14 |
|
|
|
|
|
|
116.00 |
121.50 |
5.50 |
3.52 |
|
|
|
|
|
|
118.50 |
121.00 |
2.50 |
7.35 |
|
|
|
|
|
|
124.50 |
147.00 |
22.50 |
5.13 |
|
|
|
|
|
|
132.00 |
133.00 |
1.00 |
10.93 |
|
|
|
|
|
|
136.00 |
141.00 |
5.00 |
17.35 |
|
|
|
|
|
|
152.00 |
152.50 |
0.50 |
0.06 |
|
|
|
|
|
|
156.00 |
156.50 |
0.50 |
0.06 |
|
|
|
|
|
|
163.50 |
168.50 |
5.00 |
0.08 |
|
|
|
|
|
|
178.50 |
187.00 |
8.50 |
0.05 |
|
|
|
|
|
|
190.00 |
192.00 |
2.00 |
0.11 |
|
|
PLS18-588 |
645E |
338 |
-69.4 |
115.50 |
166.00 |
50.50 |
8.21 |
|
|
|
|
|
|
142.50 |
158.00 |
15.50 |
23.89 |
|
|
|
|
|
|
170.50 |
177.00 |
6.50 |
0.27 |
|
|
|
|
|
|
181.00 |
183.00 |
2.00 |
0.06 |
|
|
|
|
|
|
188.50 |
200.50 |
12.00 |
0.23 |
|
|
|
|
|
|
205.50 |
206.00 |
0.50 |
0.12 |
|
|
|
|
|
|
219.50 |
224.50 |
5.00 |
0.09 |
|
|
PLS18-589 |
675E |
338 |
-69.6 |
117.00 |
121.50 |
4.50 |
0.15 |
|
|
|
|
|
|
137.50 |
175.50 |
38.00 |
1.49 |
|
|
|
|
|
|
147.00 |
153.50 |
6.50 |
7.26 |
|
|
|
|
|
|
178.50 |
179.00 |
0.50 |
0.26 |
|
|
|
|
|
|
185.50 |
188.00 |
2.50 |
0.27 |
|
|
|
|
|
|
192.50 |
195.00 |
2.50 |
0.12 |
|
|
|
|
|
|
198.00 |
203.50 |
5.50 |
0.39 |
|
|
|
|
|
|
207.00 |
209.00 |
2.00 |
0.13 |
|
|
PLS18-590 |
555E |
335 |
-69.8 |
111.00 |
111.50 |
0.50 |
0.10 |
|
|
|
|
|
|
117.50 |
143.50 |
26.00 |
2.12 |
|
|
|
|
|
|
134.50 |
143.50 |
9.00 |
5.28 |
|
|
|
|
|
|
151.50 |
153.00 |
1.50 |
0.74 |
|
|
|
|
|
|
156.00 |
160.00 |
4.00 |
2.59 |
|
|
|
|
|
|
158.00 |
160.00 |
2.00 |
5.15 |
|
|
|
|
|
|
162.50 |
164.50 |
2.00 |
0.08 |
|
|
|
|
|
|
171.50 |
176.00 |
4.50 |
0.70 |
|
|
|
|
|
|
185.00 |
230.00 |
45.00 |
0.22 |
|
|
|
|
|
|
233.00 |
241.00 |
8.00 |
0.06 |
|
|
|
|
|
|
245.00 |
246.00 |
1.00 |
0.09 |
|
|
|
|
|
|
249.50 |
250.00 |
0.50 |
0.07 |
|
|
PLS18-591 |
540E |
330 |
-68.0 |
104.00 |
131.50 |
27.50 |
2.37 |
|
|
|
|
|
|
121.50 |
128.50 |
7.00 |
6.68 |
|
|
|
|
|
|
135.00 |
147.50 |
12.50 |
7.63 |
|
|
|
|
|
|
135.00 |
137.00 |
2.00 |
10.88 |
|
|
|
|
|
|
143.50 |
145.50 |
2.00 |
33.08 |
|
|
|
|
|
|
153.00 |
154.50 |
1.50 |
0.19 |
|
|
|
|
|
|
162.50 |
164.00 |
1.50 |
0.35 |
|
|
|
|
|
|
168.50 |
173.00 |
4.50 |
0.20 |
|
|
|
|
|
|
175.50 |
176.50 |
1.00 |
0.43 |
|
|
|
|
|
|
181.50 |
190.00 |
8.50 |
0.36 |
|
|
|
|
|
|
192.50 |
203.00 |
10.50 |
0.06 |
|
|
|
|
|
|
207.50 |
224.00 |
16.50 |
0.43 |
|
|
|
|
|
|
211.50 |
212.50 |
1.00 |
1.58 |
|
|
|
|
|
|
230.00 |
231.00 |
1.00 |
0.06 |
Composite Parameters
- Minimum Thickness: 0.50m
- Grade Cut-Off: 0.05 U3O8 (wt%)
- Maximum Internal Dilution: 2.00m
Composited % U3O8 mineralized intervals are summarized in Table 1. Samples from the drill
core are split in half sections on site. Where possible, samples are standardized at 0.5m down-hole intervals. One-half of the
split sample is sent to SRC Geoanalytical Laboratories (an SCC ISO/IEC 17025: 2005 Accredited Facility) in Saskatoon, SK for
analysis which includes U3O8 (wt %) and fire assay for gold, while the other half remains on site for
reference. All analysis includes a 63 element ICP-OES, uranium by fluorimetry and boron. All depths reported of core interval
measurements including sample and interval widths are down-hole and are not always representative of true thickness. The
orientation of the mineralized intervals tend to follow that of lithologic contacts, and generally dip steeply to the south. Within
the Triple R deposit, individual zone wireframe models constructed from assay data and used in the resource estimate indicate that
all 5 zones have a complex geometry controlled by and parallel to steeply south-dipping lithological boundaries as well as a
preferential sub-horizontal orientation.
PLS Mineralized Trend & Triple R Deposit Summary
Uranium mineralization of the Triple R deposit at PLS occurs within the Patterson Lake Conductive Corridor and
has been traced by core drilling over ~3.18km of east-west strike length in five separated mineralized "zones" which collectively
make up the Triple R deposit. From west to east, these zones are: R1515W, R840W, R00E, R780E and R1620E. Through successful
exploration programs completed to date, Triple R has evolved into a large, near surface, basement hosted, structurally controlled
high-grade uranium deposit. The discovery hole was announced on November 05, 2012 with drill hole PLS12-022, from what is now
referred to as the R00E zone.
The R1515W, R840W and R00E zones make up the western region of the Triple R deposit and are located on land,
where overburden thickness is generally between 55m to 100m. R1515W is the western-most of the zones and is drill defined to
~90m in strike-length, ~68m across strike and ~220m vertical and where mineralization remains open in several directions.
R840W is located ~515m to the east along strike of R1515W and has a drill defined strike length of ~430m. R00E is located
~485m to the east along strike of R840W and is drill defined to ~115m in strike length. The R780E zone and R1620E zones make
up the eastern region of the Triple R deposit. Both zones are located beneath Patterson Lake where water depth is generally
less than six metres and overburden thickness is generally about 50m. R780E is located ~225m to the east of R00E and has a
drill defined strike length of ~945m. R1620E is located ~210m along strike to the east of R780E, and is drill defined to
~185m in strike length.
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 volcanic rocks with varying
degrees of alteration. Mineralization is both located within and associated with mafic volcanic 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 Fission Uranium Corp. PLS is accessible by road
with primary access from all-weather Highway 955, which runs north to the former Cluff Lake mine and passes through the nearby
UEX-Areva Shea Creek discoveries located 50km to the north, currently under active exploration and development.
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 Ross McElroy, P.Geol., President and
COO for Fission Uranium Corp., a qualified person.
About Fission Uranium Corp.
Fission Uranium Corp. is a Canadian based resource company specializing in the strategic exploration and
development of the Patterson Lake South uranium property - host to the class-leading Triple R uranium deposit - and is
headquartered in Kelowna, British Columbia. Fission’s common shares are listed on the TSX Exchange under the symbol "FCU" and
trade on the OTCQX marketplace in the U.S. under the symbol "FCUUF."
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 Fission and Fission Uranium 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.sedar.com. The forward-looking statements
included in this press release are made as of the date of this press release and the Company and Fission Uranium disclaim 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.
