Li-FT Power Ltd. (“
LIFT” or the
“
Company”) (
TSXV: LIFT)
(
OTCQX: LIFFF) (
Frankfurt:
WS0) is pleased to report assays from 8 drill
holes completed at the Fi Southwest, BIG West, Nite, & Fi Boye
pegmatites within the Yellowknife Lithium Project (“YLP”) located
outside the city of Yellowknife, Northwest Territories (Figure 1).
Drilling intersected significant intervals of spodumene
mineralization, with the following highlights:
Highlights:
- YLP-0199: 22 m at 1.05%
Li2O, (Fi
Southwest) including: 9 m at 1.87% Li2O
- YLP-0195:
15 m at 1.0%
Li2O,
(Nite)including: 2 m at 1.42% Li2Oand including: 8 m at
1.26% Li2O
-
YLP-0189: 4 m at 1.11%
Li2O, (Fi Boye)
Discussion of Results
This week’s drill results are from 1,325 m
drilled across eight holes, including the first hole of the 2024
winter program at Fi Southwest as well as 2023 results from the
Nite, BIG West, and Fi Boye pegmatites. A table of composite
calculations, general comments related to this discussion, and a
table of collar headers are provided towards the end of this
section.
David Smithson, SVP, Geology of LIFT comments,
“Results from the deep drilling at Nite this week continue to
impress with hole 195 intercepting 15 m at 1.0% Li2O at 250 m from
the surface. This is the second deep hole we have drilled on the
Nite structure following on from 10 m at 1.4% Li2O drilled at the
same level in 2023. The Fi Southwest dyke was similarly impressive
this week returning 22 m at 1.0% Li2O near to the surface. Drilling
to date on the Fi Southwest dyke has defined over 900 m of good
shallow mineralization so we are very excited to test the rest of
the structure to depth in the 2024 drill program currently underway
in the field.”
Figure 1 – Location of LIFT’s Yellowknife
Lithium Project. Drilling has been thus far focused on the Near
Field Group of pegmatites which are located to the east of the city
of Yellowknife along a government-maintained paved highway, as well
as the Echo target in the Further Afield Group.
The Fi-SW dyke strikes over at least 1.1 km on
surface with an average outcropping width of approximately 20 m.
The dyke dips between 60°-80° to the east-southeast and trends
towards the north-northeast. Drilling of Fi SW shows that it ranges
from a single 20-40 m wide dyke to 2-3 dykes of similar cumulative
width within a 50-70 m wide corridor.
YLP-0199 is the first hole drilled in the 2024
winter program and was collared to test the Fi SW pegmatite
approximately 150 m from its northern mapped extent and 50 m
beneath the surface. Drilling intersected 4 m and 15 m wide
pegmatites separated by 3 m of country rock with assays returning a
wall-to-wall composite of 1.05% Li2O over 22 m that includes 9 m of
1.87% Li2O (Table 1 & 2, Figures 2 & 3).
Figure 2 – Plan view showing the surface
expression of the Fi Southwest pegmatite with diamond drill holes
reported in this press release.
Figure 3 – Cross-section illustrating YLP-0199
with results as shown in the Fi Southwest pegmatite dyke with a 22
m interval of 1.05% Li2O.
Nite Pegmatite
The Nite pegmatite complex comprises a
north-northeast trending corridor of parallel-trending dykes that
is exposed for at least 1.4 km of strike length and dips
approximately 50°-70° degrees to the east. The northern part of
this complex consists of a main dyke flanked by one or more thinner
dykes whereas the southern part comprises a fanning splay of 5-10
thinner dykes that is up to 200 m wide.
YLP-0192 explored the Nite pegmatite
approximately 400 m from its northern end, 150 m beneath the
surface, and 100 m downdip of previously released YLP-0152 (1.24%
Li2O over 5 m). Drilling intersected five pegmatite dykes ranging
from 1-7 m wide for cumulative pegmatite of 19 m over 45 m of core.
The deepest of these three dykes returned 0.87% Li2O over 6 m that
includes 2 m of 1.99% Li2O.
YLP-0195 was drilled on a section 300 m south of
YLP-0192 to test the Nite pegmatite 700 m from its northern end,
250 m beneath the surface, and 200 m downdip of YLP-0138 (1.51%
Li2O over 12 m). New drilling intersected a 17 m wide dyke flanked
by several 1-8 m dykes for cumulative 28 m of pegmatite over 59 m
of core. Sampling of the thick dyke returned an assay composite of
1.00% Li2O over 15 m that includes subintervals of 1.42% Li2O over
2 m and 1.26% Li2O over 8 m (Table 1 & 2, Figures 4 &
5).
Figure 4 – Plan view showing the surface
expression of the Nite pegmatite with diamond drill holes reported
in this press release.
Figure 5 – Cross-section of YLP-0195 which
intersected the Nite pegmatite dyke with a 15 m interval of 1.00%
Li2O.
BIG West Pegmatite
The BIG West pegmatite complex comprises a
northeast-trending corridor of parallel-trending dykes that is
exposed for at least 1.5 km along strike and is steeply west
dipping to subvertical. The complex is bound by two relatively
continuous dyke structures that are 50-100 m apart in the northern
half of the corridor and 150 m apart in the south. These dykes are
here referred to as the east- (EB) and west-bounding (WB) dykes.
This week’s results are described from southern- to
northern-most.
YLP-0180 tested the WB dyke approximately 450 m
from its southern mapped extent and <25 m beneath the surface,
as well as 50 m and 100 m up-dip of previously released holes
(YLP-0160, 0164) that both returned negligible grades. Drilling
intersected a single 11 m wide pegmatite dyke that returned an
assay composite of 0.54% Li2O over 5 m, which includes 1 m of 1.60%
Li2O.
YLP-0185 was collared just west of the EB dyke
and 200 m from the northern mapped extent of the BIG West complex
to target the WB dyke approximately 50 m beneath the surface and
100 m up-dip of YLP-0191 (see below). Drilling intersected a single
one-metre-wide pegmatite dyke that returned negligible grade.
YLP-0191 was drilled on the same section as
YLP-0185 but was collared just east of the EB dyke, so that it
tested this dyke within 25-50 m of the surface and the WB dyke at
150 m depth. Drilling shows that these bounding dykes are separated
by ~100 m of country rock, with the EB dyke comprising two 11-12 m
dykes flanked by 2-3 m wide dykes for cumulative 28 m of pegmatite
over 70 m of drill core whereas WB comprises a single 27 m wide
dyke. Significant assays were returned only from the EB dyke and
includes composites of 0.74% Li2O over 11 m (including 1.48% Li2O
over 4 m) and 0.54% Li2O over 12 m (with 1.44% Li2O over 3 m).
YLP-0183 is the most northerly hole drilled on
the BIG West complex in 2023, just ~150 m from its northern mapped
extent and targeting the EB dyke within 25 m of the surface.
Drilling intersected a 13 m wide dyke flanked by several 1-7 m wide
dykes for 33 m of pegmatite over 69 m of drill core. Assays from
the thick dyke returned a composite of 0.51% Li2O over 6 m that
includes a 1 m interval of 1.16% Li2O whereas the flanking dykes
returned negligible grade (Table 1 & 2, Figures 6 & 7).
Figure 6 – Plan view showing the surface
expression of the BIG West pegmatite with diamond drill holes
reported in this press release.
Figure 7 – Cross-section of YLP-0191 which
intersected the BIG West pegmatite dyke with a 11 m interval of
0.74% Li2O.
Fi Boye Pegmatite
The Fi Boye pegmatite comprises a corridor of
mostly north-south striking, steeply east-dipping, dykes that run
parallel to, and lie 500-700 m west of, the Fi Main complex. The Fi
Boye corridor has at least 1.7 km of striking length, contains
between 1-5 dykes, and ranges from approximately 10-200 m in width.
The two holes reported below comprise all the drilling done on Fi
Boye in 2023.
YLP-0189 was drilled to test the Fi Boye dyke
approximately 200 m from its northern mapped extent and 50 m
beneath the surface. Drilling intersected a 14 m wide dyke flanked
by several 1-2 m wide dykes for cumulative pegmatite of 16 m over
31 m. The thick dyke returned an assay composite of 1.11% Li2O over
4 m (Table 1 & 2, Figure 8).
Figure 8 – Plan view showing the surface
expression of the Fi Boye pegmatite with diamond drill holes
reported in this press release.
Table 1 – Assay highlights for drill
holes reported in this press release.
Hole No. |
From (m) |
To (m) |
Interval (m) |
Li2O% |
Dyke |
YLP-0180 |
10 |
15 |
5 |
0.54 |
BIG West |
inc |
13 |
14 |
1 |
1.60 |
YLP-0183 |
18 |
24 |
6 |
0.51 |
BIG West |
inc |
21 |
22 |
1 |
1.16 |
YLP-0185 |
No significant results |
BIG West |
YLP-0189 |
15 |
19 |
4 |
1.11 |
Fi Boye |
YLP-0191 |
27 |
38 |
11 |
0.74 |
BIG West |
inc |
29 |
33 |
4 |
1.48 |
and |
71 |
83 |
12 |
0.54 |
inc |
72 |
75 |
3 |
1.44 |
YLP-0192 |
176 |
182 |
6 |
0.87 |
Nite |
Inc |
178 |
180 |
2 |
1.99 |
YLP-0195 |
311 |
326 |
15 |
1.00 |
Nite |
inc |
311 |
313 |
2 |
1.42 |
and inc |
318 |
326 |
8 |
1.26 |
YLP-0199 |
58 |
80 |
22 |
1.05 |
Fi SW |
inc |
66 |
75 |
9 |
1.87 |
Drilling Progress Update
The Company has concluded its 2023 drill program
at the Yellowknife Lithium Project with 34,238 m completed.
Currently, LIFT has reported results from 189 out of 198 diamond
drill holes (33,309 m).
General Statements
Six of the eight holes described in this news
release were drilled broadly perpendicular to the dyke orientation
so that the true thickness of reported intercepts will range
somewhere between 65-100% of the drilled widths. A collar header
table is provided below.
Two of the three holes drilled at the north end
of the BIG West complex (YLP-0185, 0191) were drilled broadly
downdip because collar locations for drilling perpendicular to dyke
orientation fall within Big Hill Lake. The true thickness of these
downdip intercepts will range between 40-50% of the drilled
widths.
Mineralogical characterization for the YLP
pegmatites is in progress through hyperspectral core scanning and
X-ray diffraction work. Visual core logging indicates that the
predominant host mineral is spodumene.
Table 2 - Drill collars table of reported
drill holes in this press release
Drill Hole |
NAD83 |
Easting |
Northing |
Elevation (m) |
Azimuth (°) |
Dip (°) |
Depth (m) |
Dyke |
YLP-0180 |
Zone 11 |
653,779 |
6,933,153 |
208 |
115 |
45 |
41 |
BIG West |
YLP-0183 |
Zone 11 |
654,217 |
6,933,778 |
204 |
115 |
45 |
87 |
BIG West |
YLP-0185 |
Zone 11 |
654,202 |
6,933,730 |
206 |
298 |
45 |
102 |
BIG West |
YLP-0189 |
Zone 12 |
371,157 |
6,942,629 |
253 |
84 |
45 |
141 |
Fi Boye |
YLP-0191 |
Zone 11 |
654,251 |
6,933,702 |
202 |
295 |
45 |
237 |
BIG West |
YLP-0192 |
Zone 11 |
647,717 |
6,936,538 |
203 |
298 |
50 |
255 |
Nite |
YLP-0195 |
Zone 11 |
647,678 |
6,936,208 |
215 |
298 |
52 |
360 |
Nite |
YLP-0199 |
Zone 12 |
371,462 |
6,941,023 |
251 |
302 |
46 |
102 |
Fi SW |
QA/QC & Core Sampling Protocols
All drill core samples were collected under the
supervision of LIFT employees and contractors. Drill core was
transported from the drill platform to the core processing facility
where it was logged, photographed, and split by diamond saw prior
to being sampled. Samples were then bagged, and blanks and
certified reference materials were inserted at regular intervals.
Field duplicates consisting of quarter-cut core samples were also
included in the sample runs. Groups of samples were placed in large
bags, sealed with numbered tags to maintain a chain-of-custody, and
transported from LIFT’s core logging facility to ALS Labs (“ALS”)
laboratory in Yellowknife, Northwest Territories.
Sample preparation and analytical work for this
drill program were carried out by ALS. Samples were prepared for
analysis according to ALS method CRU31: individual samples were
crushed to 70% passing through 2 mm (10 mesh) screen; a 1,000-gram
sub-sample was riffle split (SPL-21) and then pulverized (PUL-32)
such that 85% passed through 75-micron (200 mesh) screen. A
0.2-gram sub-sample of the pulverized material was then dissolved
in a sodium peroxide solution and analysed for lithium according to
ALS method ME-ICP82b. Another 0.2-gram sub-sample of the pulverized
material was analysed for 53 elements according to ALS method
ME-MS89L. All results passed the QA/QC screening at the lab, all
inserted standards and blanks returned results that were within
acceptable limits.
Qualified Person
The disclosure in this news release of
scientific and technical information regarding LIFT’s mineral
properties has been reviewed and approved by Ron Voordouw, Ph.D.,
P.Geo., Partner, Director Geoscience, Equity Exploration
Consultants Ltd., and a Qualified Person as defined by National
Instrument 43-101 Standards of Disclosure for Mineral Projects (NI
43-101) and member in good standing with the Northwest Territories
and Nunavut Association of Professional Engineers and Geoscientists
(NAPEG) (Geologist Registration number: L5245).
About LIFT
LIFT is a mineral exploration company engaged in
the acquisition, exploration, and development of lithium pegmatite
projects located in Canada. The Company’s flagship project is the
Yellowknife Lithium Project located in Northwest Territories,
Canada. LIFT also holds three early-stage exploration properties in
Quebec, Canada with excellent potential for the discovery of buried
lithium pegmatites, as well as the Cali Project in Northwest
Territories within the Little Nahanni Pegmatite Group.
For further information, please
contact:
Francis MacDonaldChief Executive OfficerTel:
+1.604.609.6185Email: info@li-ft.comWebsite: www.li-ft.com |
Daniel GordonInvestor RelationsTel: +1.604.609.6185Email:
investors@li-ft.com |
Cautionary Statement Regarding Forward-Looking
Information
Certain statements included in this press
release constitute forward-looking information or statements
(collectively, “forward-looking statements”), including those
identified by the expressions “anticipate”, “believe”, “plan”,
“estimate”, “expect”, “intend”, “may”, “should” and similar
expressions to the extent they relate to the Company or its
management. The forward-looking statements are not historical facts
but reflect current expectations regarding future results or
events. This press release contains forward looking statements.
These forward-looking statements and information reflect
management's current beliefs and are based on assumptions made by
and information currently available to the company with respect to
the matter described in this new release.
Forward-looking statements involve risks and
uncertainties, which are based on current expectations as of the
date of this release and subject to known and unknown risks and
uncertainties that could cause actual results to differ materially
from those expressed or implied by such statements. Additional
information about these assumptions and risks and uncertainties is
contained under "Risk Factors and Uncertainties" in the Company's
latest annual information form filed on March 30, 2023, which
is available under the Company's SEDAR+ profile
at www.sedarplus.ca, and in other filings that the Company has
made and may make with applicable securities authorities in the
future. Forward-looking statements contained herein are made only
as to the date of this press release and we undertake no obligation
to update or revise any forward-looking statements whether as a
result of new information, future events or otherwise, except as
required by law. We caution investors not to place considerable
reliance on the forward-looking statements contained in this press
release.
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 news release.
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