Li-FT Power Ltd. (“
LIFT” or the
“
Company”) (
TSXV: LIFT)
(
OTCQX: LIFFF) (
Frankfurt:
WS0) is pleased to report assays from 5 drill
holes completed at the Ki, Shorty, BIG East and Fi-SW pegmatites
within the Yellowknife Lithium Project (“YLP”) located outside the
city of Yellowknife, Northwest Territories (Figure 1). Drilling has
intersected significant intervals of spodumene mineralization, with
the following highlights:
Highlights:
- YLP-0087: 21 m at 1.12%
Li2O, (Ki)including: 11
m at 1.70% Li2O
- YLP-0091: 17 m at 1.28%
Li2O, (Shorty)
and:
16 m at 1.01% Li2Oincluding: 5 m at 1.55% Li2O
- YLP-0085: 13 m at 1.34%
Li2O, (BIG East)
and:
8 m at 0.86% Li2O
and: 4 m at 1.47% Li2O
and: 3 m at 1.09%
Li2O
- YLP-0084: 10 m at 1.58%
Li2O, (BIG East)
and:
4 m at 1.44% Li2O
and: 6 m at 1.19% Li2O
Francis MacDonald, CEO of LIFT comments, “Drill
intersects from this week’s results at Ki are the widest to date
with excellent grades. The northern portion of Shorty, where two
arms of the pegmatite have been structurally juxtaposed, has
benefits from an open pit mining perspective. BIG East continues to
deliver excellent widths in grades across the pegmatite dyke
system. We continue to be pleased with the consistency of excellent
drill intersects produced across the YLP portfolio.”
Discussion of Results
This week’s drill results are for five holes
from four different pegmatite dykes, including BIG East (YLP-0084,
85), Ki (YLP-0087), Fi Southwest (YLP-0090), and Shorty (YLP-0091).
A table of composite calculations, some general comments related to
this discussion, and a table of collar headers are provided towards
the end of this section.
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 that occur within a longer north-of-northwest trending
corridor. The Ki dyke itself extends for at least 1,000 m on
surface and 100 m downdip, is around 20 m thick, and dips between
65°-80° to the southwest. Typically, the Ki pegmatite consists of a
thick central dyke flanked by one or more narrower (1-5 m wide)
dykes.
YLP-0087 was designed to test the Ki pegmatite
approximately 400 m from its southeastern end and 50 m vertically
beneath the surface. Drilling intersected a 21 m wide pegmatite
flanked by 1 m wide dykes on either side, with the thicker central
pegmatite returning an assay composite of 21 m at 1.12% Li2O m that
includes 11 m at 1.70% Li2O. The two flanking dykes returned
negligible grade (Table 1 & 2, Figures 2 & 3).
Figure 2 – Plan view showing the surface
expression of the Ki pegmatite with diamond drill hole reported in
this press release.
Figure 3 – Cross-section of YLP-0087 which
intersected the Ki pegmatite dyke with a 21 m interval of 1.12%
Li2O.
Shorty Pegmatite
The Shorty pegmatite is one of several dykes
occurring within a broader north-of-northeast striking corridor.
Shorty itself comprises a braided zone of dykes that dips 50°-70°
to the west-northwest and extends for at least 700 m on surface and
200 m downdip. LIFT drilling shows that this pegmatite may comprise
a single dyke up to 25 m wide or 2-4 dykes between 1-20 m wide
occurring over 30-90 m of core length.
YLP-0091 was designed to test the northern end
of the Shorty pegmatite where it comprises two thick en échelon
dykes. The western dyke was intersected approximately 100 m from
its southern end and 50 m vertically below the surface whereas the
eastern one was cut at 100 m from its northern mapped extent and
100 m beneath the surface. Drilling showed that these dykes are
each 20 m in core width and separated by 54 m of country rock.
Assay composites for the western dyke returned 1.28% Li2O over 17 m
whereas the eastern one ran 1.01% Li2O over 16 m with a subinterval
of 1.55% Li2O over 5 m (Table 1 and 2, Figures 4 & 5).
Figure 4 – Plan view showing the surface
expression of the Shorty pegmatite with diamond drill hole reported
in this press release.
Figure 5 – Cross-section illustrating YLP-0091
with results as shown in the Shorty pegmatite dyke with a 17 m
interval of 1.28% Li2O.
BIG East
The BIG East pegmatite swarm comprises a 35-90 m
wide corridor of parallel-trending dykes that dips around 55°-75°
degrees west and extends for at least 1,300 m along surface and 200
m downdip.
YLP-0084 was designed to test the BIG East swarm
approximately 600 m from its southern mapped extent and 25 m
vertically beneath the surface. Drilling intersected seven
pegmatite dykes over 75 m of core length, with dykes ranging from
1-10 m in width for a cumulative total of 25 m. All seven dykes
returned at least one assay >0.6% Li2O with some of the better
composite intervals including 1.58% Li2O over 10 m, 1.19% Li2O over
6 m, and 1.44% Li2O over 4 m.
YLP-0085 was drilled on the same section as
YLP-0084 but centered at 75 m vertically beneath the surface.
Drilling intersected five pegmatite dykes over 66 m of core length,
with dykes ranging from 2-13 m in width for cumulative core width
of 26 m. All five dykes returned at least one assay >1.00% Li2O
with some of the better composite intervals including 1.34% Li2O
over 13 m, 0.86% Li2O over 8 m, and 1.47% Li2O over 4 m (Table 1
and 2, Figures 6 & 7).
Figure 6 – Plan view showing the surface
expression of the BIG East pegmatite with diamond drill holes
reported in this press release.
Figure 7 – Cross-section illustrating YLP-0085
and YLP-0084 with results as shown in the BIG East pegmatite dyke
with a 13 m interval of 1.34% Li2O and a 10 m interval of 1.58%
Li2O.
Fi Southwest
The Fi Southwest (SW) pegmatite is one of
several dykes occurring within a longer and wider
north-of-northeast striking dyke corridor. The Fi SW dyke comprises
a single dyke with a width of 25-40 m wide or 2-3 dykes within a
50-70 m wide corridor, and dips 60°-80° to the east-southeast as
well as extending for at least 1,100 m on surface and 200 m
downdip.
YLP-0090 was drilled to test the Fi SW pegmatite
just beyond its’ northern-most mapped extent and 50 m vertically
below the surface. Drilling intersected three, 2-7 m wide,
pegmatite dykes over 94 m of core length with cumulative pegmatite
thickness of 13 m. No significant assay results were returned.
Table 1 – Assay highlights for drill
holes reported in this press release.
Hole No. |
From (m) |
To (m) |
Interval (m) |
Li2O% |
Dyke |
YLP0084 |
7 |
17 |
10 |
1.58 |
BIG East |
and |
34 |
38 |
4 |
1.44 |
BIG East |
and |
61 |
67 |
6 |
1.19 |
BIG East |
YLP0085 |
58 |
71 |
13 |
1.34 |
BIG East |
and |
81 |
89 |
8 |
0.86 |
BIG East |
and |
101 |
105 |
4 |
1.47 |
BIG East |
and |
112 |
115 |
3 |
1.09 |
BIG East |
YLP0087 |
69 |
90 |
21 |
1.12 |
Ki |
inc |
72 |
83 |
11 |
1.70 |
Ki |
YLP0090 |
No significant results |
Fi SW |
YLP0091 |
42 |
59 |
17 |
1.28 |
Shorty |
and |
119 |
135 |
16 |
1.01 |
Shorty |
inc |
129 |
134 |
5 |
1.55 |
Shorty |
Drilling Progress Update
The Company has now concluded its 2023 drill
program at the Yellowknife Lithium Project with 34,238 m completed.
Currently, LIFT has reported results from 92 out of 198 diamond
drill holes (16,214 m).
General Statements
Four of the five 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. YLP-0090 was
drilled parallel to the dip direction of the dyke but returned
negligible grade. A collar header table is provided below.
Mineralogical characterization for the YLP
pegmatites is in progress through hyper spectral core scanning and
X-ray diffraction work. Visual core logging indicates that the
predominant host mineral is spodumene whereas other significant
non-lithium bearing phases include quartz and feldspar.
Table 2 - Drill collars table of reported
drill holes in this press release
Drill Hole |
Easting |
Northing |
Elevation (m) |
Azimuth (°) |
Dip (°) |
Depth (m) |
Dyke |
YLP0084 |
6,932,862 |
345,966 |
208 |
120 |
45 |
98 |
BIG East |
YLP0085 |
6,932,882 |
345,924 |
202 |
120 |
47 |
140 |
BIG East |
YLP0087 |
6,942,625 |
373,215 |
256 |
56 |
46 |
105 |
Ki |
YLP0090 |
6,941,161 |
371,417 |
252 |
115 |
45 |
150 |
Fi SW |
YLP0091 |
6,938,293 |
372,916 |
250 |
124 |
60 |
150 |
Shorty |
QAQC
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
MacDonald |
|
Daniel Gordon |
Chief Executive Officer |
|
Investor Relations |
Tel: + 1.604.609.6185 |
|
Tel: +1.604.609.6185 |
Email: info@li-ft.com |
|
Email: investors@li-ft.com |
Website: www.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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