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 BIG West, Nite & Ki 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-0165: 23 m at 1.25%
Li2O, (Ki)
- YLP-0150: 13 m at
1.27% Li2O, (BIG
West)
- YLP-0166: 9.5 m at 1.36%
Li2O, (BIG West)
- YLP-0157: 9 m at 1.10%
Li2O, (Nite)and: 1 m at
1.13% Li2Oand: 2 m at 0.85% Li2O
- YLP-0158: 9 m at 1.02%
Li2O, (BIG West)and: 7 m
at 1.09% Li2O
Discussion of Results
This week’s drill results are for eight holes
drilled on three separate pegmatite complexes, including BIG West,
Nite and Ki. 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.
Francis MacDonald, CEO of LIFT comments, “This
week we have released an excellent result from the Ki pegmatite.
Hole YLP-0165 is one of the better holes to date in terms of grade
x thickness. The Ki pegmatite will be one of the focuses for the
winter drill program and we plan to systematically step out from
current drilling along untested spodumene-bearing outcrops to the
northwest of drilling completed to date.”
Figure 1 – Location of LIFT’s Yellowknife
Lithium Project. Drilling has been thus far focused on the Road
Access 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.
Ki Pegmatite
The Ki pegmatite is one of several subparallel
dykes occurring within a north-of-northwest trending corridor.
Drill intercepts typically comprise a thick “main” dyke flanked by
one or more narrower (1-5 m wide) dykes although, in places, it is
formed by 2-6 dykes of similar cumulative thickness spread over up
to 80 m of core length. The Ki dyke is visible for at least 1.0 km
on surface and dips between 65°-80° to the southwest.
YLP-0165 tested the Ki pegmatite approximately
200 m from its southern mapped extent and 50 m vertically beneath
the surface, as well as 50 m down-dip of YLP-0118 (0.96% Li2O over
1 m). Drilling intersected a 23 m wide pegmatite dyke that returned
1.25% Li2O over 23 m (Table 1 & 2, Figures 2 & 3).
Figure 2 – Plan view showing the surface
expression of the Ki pegmatite with diamond drill holes reported in
this press release.
Figure 3 – Cross-section illustrating YLP-0165
with results as shown in the Ki pegmatite dyke with a 23 m interval
of 1.25% 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 dykes that are 50-100 m apart in the northern half of
the corridor and 150 m apart in the south. To facilitate
description, these dykes are here referred to as the east bounding
(EB) and west bounding (WB) dykes. The holes described below are
ordered from southern- to northern-most.
YLP-0163 was drilled ~200 m from the southern
mapped extent of the WB dyke and designed to test a pierce point
approximately 50 m vertically below the surface. Drilling
intersected a single 9 m wide pegmatite dyke that returned 0.99%
Li2O over 9 m.
YLP-0158 was collared 50 m north of YLP-0163 to
test the WB dyke ~250 m from its southern mapped extent and 50 m
beneath the surface. Drilling intersected 16 m of pegmatite that is
more-or-less split in half by a 5 m thick panel of country rock.
The upper interval returned an assay composite of 1.09% Li2O over 7
m whereas the lower one ran 1.02% Li2O over 9 m.
YLP-0166 was drilled on the same section as
YLP-0158 but aimed to intersect the WB dyke at a shallower depth.
Drilling intersected a single pegmatite dyke, extending from the
base of overburden to 13 m depth, that returned an assay composite
of 1.36% Li2O over 9.5 m.
YLP-0150 was collared 50 m north of
YLP-0158/0166 to test the WB dyke approximately 300 m from its
southern mapped extent and 50 m vertically below the surface.
Drilling intersected a single 14 m pegmatite dyke that returned an
assay composite of 1.27% Li2O over 13 m.
YLP-0160 was collared 150 m north of YLP-0150 to
test the WB dyke approximately 450 m from its southern mapped
extent and, again, 50 m vertically beneath the surface. Drilling
intersected five pegmatite dykes over a 70 m interval of drill core
that each range between 1-6 m in width and sum to 16 m. No
significant assays were returned.
YLP-0159 was drilled 600-850 m north of the five
holes described above, approximately 300 m from the northern mapped
extent of the WB dyke and 50 m below the surface. Drilling
intersected four dykes over a 35 m interval of drill core that each
range between 1-7 m in width and sum to 14 m of pegmatite. The only
notable assays were returned for the second dyke, which ran 0.73%
Li2O over 5 m including one meter at 1.48% Li2O (Table 1 & 2,
Figures 4, 5 & 6).
Figure 4 – Plan view showing the surface
expression of the BIG West pegmatite with diamond drill holes
reported in this press release.
Figure 5 – Cross-section of YLP-0150 which
intersected the BIG West pegmatite dyke with a 13 m interval of
1.27% Li2O.
Figure 6 – Cross-section of YLP-0166 which
intersected the BIG West pegmatite dyke with a 9.5 m interval of
1.36% 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, ranges from 10-200
m wide, and dips approximately 50°-70° to the east.
YLP-0157 was designed to test the Nite pegmatite
approximately 500 m from its northern mapped extent and 100 m
vertically beneath the surface, as well as 50 m downdip of YLP-0149
(1.04% Li2O over 5 m and 0.78% Li2O over 10 m) and 100 m downdip of
YLP-0145 (1.28% Li2O over 10 m). Drilling intersected three dykes
over a 35 m interval of core, with dykes ranging from 4-9 m in
width and summing to 17 m of pegmatite. Assay composites, from
upper- to lower-most, include 1.13% Li2O over 1 m, 1.10% Li2O over
9 m and 0.85% Li2O over 2 m (Table 1 & 2, Figure 7).
Figure 7 – Plan view showing the surface
expression of the Nite 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-0150 |
64 |
77 |
13 |
1.27 |
BIG West |
YLP-0157 |
172 |
173 |
1 |
1.13 |
Nite |
and |
183 |
192 |
9 |
1.10 |
Nite |
and |
203 |
205 |
2 |
0.85 |
Nite |
YLP-0158 |
59 |
66 |
7 |
1.09 |
BIG West |
and |
71 |
80 |
9 |
1.02 |
BIG West |
YLP-0159 |
85 |
90 |
5 |
0.73 |
BIG West |
inc |
87 |
88 |
1 |
1.48 |
BIG West |
YLP-0160 |
No significant results |
BIG West |
YLP-0163 |
69 |
78 |
9 |
0.99 |
BIG West |
YLP-0165 |
61 |
84 |
23 |
1.25 |
Ki |
YLP-0166 |
2 |
11 |
9.5 |
1.36 |
BIG West |
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 164 out of 198 diamond
drill holes (28,903 m).
General Statements
All 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.
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-0150 |
Zone 11 |
653,658 |
6,933,054 |
207 |
118 |
45 |
92 |
BIG West |
YLP-0157 |
Zone 11 |
647,675 |
6,936,437 |
206 |
300 |
52 |
222 |
Nite |
YLP-0158 |
Zone 11 |
653,651 |
6,933,003 |
205 |
118 |
50 |
101 |
BIG West |
YLP-0159 |
Zone 11 |
654,122 |
6,933,659 |
204 |
115 |
45 |
111 |
BIG West |
YLP-0160 |
Zone 11 |
653,723 |
6,933,189 |
214 |
118 |
45 |
122 |
BIG West |
YLP-0163 |
Zone 11 |
653,636 |
6,932,950 |
209 |
118 |
45 |
95 |
BIG West |
YLP-0165 |
Zone 12 |
373,258 |
6,942,597 |
259 |
30 |
56 |
97 |
Ki |
YLP-0166 |
Zone 11 |
653,698 |
6,932,986 |
206 |
118 |
45 |
32 |
BIG West |
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 in order 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.com Website: 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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