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 and BIG East 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-0080: 14 m at 1.50%
Li2O, (Ki)
- YLP-0089: 10 m at 1.75%
Li2O, (Shorty)
and: 5 m at 1.15% Li2O
and: 3 m at 1.51% Li2O
- YLP-0086: 14 m at 1.16%
Li2O, (BIG East)
and: 10 m at 1.45% Li2O
- YLP-0082: 15 m at 1.07%
Li2O, (Shorty)
Francis MacDonald, CEO of LIFT comments, “We are
pleased with the high-grade intersection of 14 meters at 1.50% Li2O
returned from the Ki pegmatite in this release. Previous drilling
at Ki was returning grades averaging around 0.90% Li2O, so this
increase in grade is a welcome surprise. BIG East and Shorty
continue to deliver excellent results as well.”
Discussion of Results
This week’s drill results are for five holes
from three different pegmatite dykes, including Ki (YLP-0080),
Shorty (YLP-0082, 83, 89), and BIG East (YLP-0086). 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.https://www.globenewswire.com/NewsRoom/AttachmentNg/747f7bf8-919e-4dc3-aed3-14a0a6366a49
Shorty Pegmatite
The Shorty pegmatite is one of several dykes
occurring within broader corridor that is north-of-northeast
striking. The Shorty pegmatite 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 1-15 m wide that occur over 30-40 m of core
length.
YLP-0082 was designed to test the Shorty dyke 50
m from its northern end and 25 m vertically beneath the surface.
Drilling intersected a single, 17 m wide, pegmatite dyke that
returned an assay composite of 1.07% Li2O over 15 m.
YLP-0083 was drilled 100 m north of YLP-0082 and
therefore 50 m past the northern-most mapped extent of the Shorty
pegmatite, with the aim of testing the northward extension of this
dyke at 25 m vertically beneath the surface. Drilling intersected
two dykes; an upper 1 m wide pegmatite and a lower 10 m wide dyke
that includes a 2 m panel of country rock. Assays for both dykes
returned insignificant grades.
YLP-0089 likewise tested a 50 m northward
extension of the Shorty pegmatite but at 50 m vertically beneath
the surface. Results from this hole were significantly better than
YLP-0083, with drilling cutting five 1-12 m wide dykes over a 49 m
interval of drill collar followed by a sixth, 9 m wide, dyke that
starts 33 m further down the hole. Notable assay composites include
1.15% Li2O over 5 m and 1.75% Li2O over 10 m for the two upper-most
dykes as well as 1.51% Li2O over 3 m for the lower-most one. The
three narrowest dykes, each of which ranges between 1-2 m thick,
returned negligible grades. The results of this hole are important
in confirming that mineralization extends beyond the currently
mapped extent of the Shorty pegmatite (Table 1 & 2, Figures 2,
3, & 4).
Figure 2 – Plan view showing the surface
expression of the Shorty pegmatite with diamond drill holes
reported in this press
release.https://www.globenewswire.com/NewsRoom/AttachmentNg/a1e0bb4c-e080-4d7b-9ba5-18b1fb86ec02
Figure 3 – Cross-section of YLP-0082 which
intersected the Shorty pegmatite dyke with a 15 m interval of 1.07%
Li2O.https://www.globenewswire.com/NewsRoom/AttachmentNg/8cec6fc1-0868-4043-bf61-b5684e14ed2e
Figure 4 – Cross-section of YLP-0089 which
intersected the Shorty pegmatite dyke with a 10 m interval of 1.75%
Li2O.https://www.globenewswire.com/NewsRoom/AttachmentNg/8c687746-d1fb-40bd-8e59-d6b91aa8f474
Ki Pegmatite
The Ki pegmatite is one of several dykes
occurring within a longer corridor that is broadly
north-of-northwest striking. The Ki dyke itself trends parallel to
this corridor and 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. The thicker dyke is here referred to as the main dyke
and is typically flanked by one or more narrower (1-5 m wide)
dykes.
YLP-0080 was designed to test the Ki pegmatite
150 m from its northwestern end and 25 m vertically beneath the
surface. Drilling intersected a single pegmatite that is 14 m thick
and returned a wall-to-wall assay composite of 1.50% Li2O over 14 m
(Table 1 and 2, Figures 5 & 6).
Figure 5 – Plan view showing the surface
expression of the Ki pegmatite with diamond drill hole reported in
this press
release.https://www.globenewswire.com/NewsRoom/AttachmentNg/9e542387-d49b-4160-a54d-df72c45aaf46
Figure 6 – Cross-section illustrating YLP-0080
with results as shown in the Ki pegmatite dyke with a 14 m interval
of 1.50%
Li2O.https://www.globenewswire.com/NewsRoom/AttachmentNg/a3951237-1d0c-4d86-b6ff-23b4fe6ed98f
BIG East Pegmatite
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-0086 was designed to test the BIG East swarm
450 m from its northern end and approximately 70 m vertically
beneath the surface. Drilling intersected two pegmatite dykes that
are 11 and 19 m in core length and separated from each other by 6 m
of metasedimentary country rock. The upper dyke returned an assay
composite of 1.45% Li2O over 10 m whereas the lower dyke returned
1.16% Li2O over 14 m (Table 1 and 2, Figures 7 & 8).
Figure 7 – Plan view showing the surface
expression of the BIG East pegmatite with diamond drill hole
reported in this press
release.https://www.globenewswire.com/NewsRoom/AttachmentNg/00e7ac8a-1d97-48d0-8359-71477f762b4f
Figure 8 – Cross-section illustrating YLP-0086
with results as shown in the BIG East pegmatite dyke with a 14 m
interval of 1.16%
Li2O.https://www.globenewswire.com/NewsRoom/AttachmentNg/0e137634-400c-4959-b384-2d5c3fbd1255
Table 1 – Assay highlights for drill
holes reported in this press release.
Hole No. |
From (m) |
To (m) |
Interval (m) |
Li2O% |
Dyke |
YLP-0080 |
8 |
22 |
14 |
1.50 |
Ki |
YLP-0082 |
10 |
25 |
15 |
1.07 |
Shorty |
YLP-0083 |
No significant results |
Shorty |
YLP-0086 |
60 |
70 |
10 |
1.45 |
BIG East |
and |
80 |
94 |
14 |
1.16 |
BIG East |
YLP-0089 |
8 |
13 |
5 |
1.15 |
Shorty |
and |
18 |
28 |
10 |
1.75 |
Shorty |
and |
88 |
91 |
3 |
1.51 |
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 87 out of 198 diamond
drill holes (15,333 m).
General Statements
All 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. 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 whereas other significant
non-lithium bearing phases include quartz and feldspar.
Drill Hole |
Easting |
Northing |
Elevation (m) |
Azimuth (°) |
Dip (°) |
Depth (m) |
Dyke |
YLP0080 |
373,098 |
6,942,846 |
257 |
56 |
45 |
33 |
Ki |
YLP0082 |
372,968 |
6,938,192 |
249 |
123 |
50 |
45 |
Shorty |
YLP0083 |
373,018 |
6,938,275 |
251 |
124 |
45 |
60 |
Shorty |
YLP0086 |
345,988 |
6,933,022 |
207 |
120 |
45 |
131 |
BIG East |
YLP0089 |
372,962 |
6,938,313 |
251 |
124 |
45 |
119 |
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 analyzed 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.
Li FT Power (TSXV:LIFT)
Historical Stock Chart
From Dec 2024 to Jan 2025
Li FT Power (TSXV:LIFT)
Historical Stock Chart
From Jan 2024 to Jan 2025