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LIFT intersects 35 m at 1.32% Li2O at its Shorty pegmatite, Yellowknife Lithium Project, NWT

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Li-FT Power has announced assay results from 12 drill holes at its Yellowknife Lithium Project (YLP) in the Northwest Territories. The highlights include a 35-meter interval at 1.32% Li2O at the Shorty pegmatite and an 11-meter interval at 1.16% Li2O at the Ki pegmatite. Other significant results were reported from the Echo, BIG East, and Fi Main pegmatites. These findings extend high-grade mineralization at the Shorty pegmatite to a total of 400 meters on the surface. The company recently completed its winter drilling program, totaling 49,548 meters across 286 diamond drill holes. These new intersections provide promising indications of substantial lithium resources, which could enhance the project's economic viability.

Positive
  • Interception of 35 meters at 1.32% Li2O near the surface at Shorty.
  • Extension of high-grade mineralization for 400 meters on the surface at Shorty.
  • Completion of the winter drilling program with a total of 49,548 meters.
  • Significant intercepts at multiple pegmatites including Ki and Echo.
Negative
  • Some drill holes, such as YLP-0252 and YLP-0250, returned no significant lithium mineralization.
  • Echo pegmatite results included several intervals with negligible grades of Li2O.
  • high-grade findings at the Fi Main pegmatite, with assays returning ≤0.3% Li2O.

VANCOUVER, British Columbia, May 22, 2024 (GLOBE NEWSWIRE) -- Li-FT Power Ltd. (“LIFT” or the “Company”) (TSXV: LIFT) (OTCQX: LIFFF) (Frankfurt: WS0) is pleased to report assays from 12 drill holes completed at the Shorty, BIG East, Echo, Fi Main, & 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-0283: 35 m at 1.32% Li2O, (Shorty)
  • YLP-0274: 11 m at 1.16% Li2O, (Ki)
    including: 6 m at 1.87% Li2O
  • YLP-0263: 12 m at 0.82% Li2O, (Echo)
    Including: 6 m at 1.29% Li2O

Discussion of Results

This news release provides results for 12 drill holes (1,918 m) from Li-FT’s 2024 winter drilling program. Holes are reported from five different pegmatite complexes that include Shorty, Ki, Echo, BIG East, and Fi Main. 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.

Dave Smithson, SVP Geology of LIFT comments, “Shorty continues to deliver near-surface high grade spodumene mineralization this week, with YLP-0283 returning an impressive 35 m of 1.32% Li2O only 50 m from surface. The intercept extends strong shallow mineralization drilled 100 m to the southwest in holes YLP091 & YLP097 (17 m of 1.28% Li2O, 16 m of 1.01% Li2O, and 23 m of 1.03% Li2O) from 2023. This new information extends high grade mineralization for a total of 400 m on surface at Shorty emphasising the dyke’s potential to deliver significant high-grade tonnes from surface.” 

Li-FT detailed maps yellowknife with roads March 2024

Figure 1 – Location of LIFT’s Yellowknife Lithium Project. Drilling has been thus far mainly 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, and advancing to the Echo target, the first drilling in the Further Afield Group.

Shorty Pegmatite

The Shorty pegmatite is formed by several sub-parallel dykes that, together, define a pegmatite-bearing corridor that is at least 1.4 km long, up to 100 m wide, north-northeast striking, and dips 50°-70° to the west. The corridor itself consists of both country rock and pegmatite, with pegmatite occurring as either a single 10-40 m wide dyke or as 2-4 dykes with a similar cumulative width spread over 50-100 m of core length.

YLP-0283 was collared within a few metres of the lease boundary to test the Shorty corridor at approximately 50 to 100 m below the surface and 50 m north of a section with previously released YLP-0089 (1.55% Li2O over 15 m from 2 intervals, 5 m apart). Drilling intersected a 35 m dyke centered at approximately 50 m below the surface that returned a wall-to-wall composite of 1.32% Li2O. This intersection is the northeastern-most hole drilled on Shorty corridor to date with mineralization open at depth and along strike to the north-northeast where it extends off LIFT’s claims (Table 1 & 2, Figures 2 & 3).

Individual Drill plans YK pegmatites NR 32 new shorty

Figure 2 – Plan view showing the surface expression of the Shorty pegmatite with diamond drill holes reported in this press release.

Yellowknife sections NR32 Shorty

Figure 3 – Cross-section illustrating YLP-0283 with results as shown in the Shorty pegmatite dyke with a 35 m interval of 1.32% Li2O.

Ki Pegmatite

The Ki pegmatite complex comprises a north-northwest trending corridor of dykes that extends for at least 1.3 km on surface and dips steeply to the southwest. The southern part of the corridor consists mostly of one large dyke and several narrower flanking dykes that sum to a constant pegmatite width of around 25 m. The northern part consists of two relatively thick dykes that are between 50-150 m apart, with the western dyke comprising the northern extension of the Ki dyke and the more eastern dyke referred to as Perlis.

YLP-0274 was drilled at the northern end of the Ki dyke where it overlaps with the southern end of the Perlis dyke. The hole was designed to test both dykes at depths of approximately 10 and 75 m below the surface. Drilling intersected the Ki dyke, with a width of 11 m, as well four 1 to 4 m wide dykes spread over 86 m of core further down the hole, the deepest of which is possibly Perlis. The Ki dyke returned a wall-to-wall composite of 1.16% Li2O that includes 6 m of 1.87% Li2O and is open at depth and to the north. The other dykes returned negligible grade (Table 1 & 2, Figures 4 & 5).

Individual Drill plans YK pegmatites Ki NR32 GT for May 21

Figure 4 – Plan view showing the surface expression of the Ki pegmatite with diamond drill holes reported in this press release.

Yellowknife sections NR32 Ki

Figure 5 – Cross-section illustrating YLP-0274 with results as shown in the Ki pegmatite dyke with a 11 m interval of 1.16% Li2O.

YLP-0261 was collared 150 m southeast of YLP-0274 to test the Ki corridor from approximately 5 to 75 m below the surface and 50 m north of previously released YLP-0072 (0.79% Li2O over 17 m). New drilling intersected a dyke cluster just below overburden and another centered at 75 m depth, with the shallower cluster returning a composite of 0.56% Li2O over 3 m (Table 1 & 2, Figure 4).

Echo Pegmatite

The Echo pegmatite complex comprises a steeply dipping, northwest-trending, feeder dyke (“Echo feeder”) that splits into a fanning splay of moderate to gently dipping dykes for 0.5 km to the northwest (“Echo splay”). The dyke complex has a total strike length of over 1.0 km. The feeder dyke is 10-15 m wide whereas the gently dipping dykes in the splay are thicker, ranging from 10-25 m. All six of the holes reported here were drilled on the feeder dyke and are described below from northern to southernmost.

YLP-0263 tested the Echo feeder dyke near where it merges with the Echo splay, approximately 75 m below the surface and 50 m downdip of previously released YLP-0226 (1.45% Li2O over 13 m). New drilling intersected 6 and 12 m wide dykes separated by 7 m of country rock, with the thicker dyke returning a wall-to-wall composite of 0.82% Li2O that includes 6 m of 1.29% Li2O. High grade spodumene mineralization is cut out by a mafic dyke but is open at depth and along strike to the north (Table 1 & 2, Figures 6 & 7).

Individual Drill plans YK pegmatites Echo NR32 GT for May 21

Figure 6 – Plan view showing the surface expression of the Echo pegmatite with diamond drill holes reported in this press release.

Yellowknife sections NR32 Echo

Figure 7 – Cross-section illustrating YLP-0263 with results as shown in the Echo pegmatite dyke with a 12 m interval of 0.82% Li2O.

YLP-0253 was drilled on a section 275 m south of the section with YLP-0226/0263 to test the Echo feeder at 125-150 m below the surface and 100 metres downdip of previously released YLP-0248 (0.92% Li2O over 11 m). New drilling intersected a nine-metre-wide feeder dyke that returned a composite of 0.50% Li2O over 6 m (Table 1 & 2, Figure 6).

YLP-0256 was drilled on a section 50 m south of the section with YLP-0248/0253 to test the Echo feeder approximately 25-50 m below the surface. Drilling intersected a 26 m wide corridor with 10 m of pegmatite spread over three dykes, one of which returned a composite of 0.57% Li2O over 3 m (Table 1 & 2, Figure 6).

YLP-0252 was drilled on a section an additional 50 m south to test the Echo feeder at 25-50 m below the surface and 100 m up-dip of YLP-0254 (1.23% Li2O over 6 m). New drilling intersected a 29 m wide corridor with 10 m of pegmatite spread over two dykes, neither of which returned assays over 0.1% Li2O (Table 1 & 2, Figure 6).

YLP-0257 was drilled on a section 100 m south of the previously described hole (YLP-0252) to test the Echo feeder at approximately 100 m below the surface and 75 m downdip of previously released YLP-0236 (0.79% Li2O over 7 m). New drilling intersected several 1 to 3 m wide flanking dykes at shallower depth and then a 7 m wide pegmatite interpreted as the feeder. No significant assays were returned (Table 1 & 2, Figure 6).

YLP-0244 was drilled on a section an additional 100 m south of the previously described hole to test the Echo feeder approximately 100 m from its mapped southern extent, 100 m below the surface, and 75 m downdip of previously released YLP-0245 (0.62% Li2O over 7 m). Drilling intersected a 22 m wide corridor with 11 m of pegmatite spread over two dykes, neither of which returned assays over 0.1% Li2O (Table 1 & 2, Figure 6).

BIG East Pegmatite

The BIG East pegmatite complex comprises a north-northeast trending corridor of parallel-trending dykes that is exposed for at least 1.8 km of strike length, ranges from 10-100 m wide, and dips approximately 55°-75° degrees to the west.

YLP-0267 is the northern-most hole reported from the BIG East complex to date and was drilled to test the corridor at 25-125 m below the surface on a section located 50 m north of previously released hole YLP-0262 (1.22% Li2O over 11 m). Drilling intersected a 25 m wide dyke centered at approximately 100 m below the surface and flanked by one or more 2 to 9 m wide dykes on either side. Assays returned composites of 0.46% Li2O over 3 m and 0.46% Li2O over 8 m from the thick dyke as well as 0.57% Li2O over 1 m from one of the flanking dykes (Table 1 & 2, Figures 8 & 9).

Individual Drill plans YK pegmatites Big E NR32 GT for May 21

Figure 8 – Plan view showing the surface expression of the BIG East pegmatite with diamond drill holes reported in this press release.

Yellowknife sections NR32 Big E

Figure 9 – Cross-section illustrating YLP-0267 with results as shown in the BIG East pegmatite dyke with a 8 m interval of 0.46% Li2O.

Fi Main Pegmatite

The Fi Main pegmatite complex crops out over at least 1.5 km of strike length within a north-south striking corridor that dips between 70°-85° to the west. The central 800-900 m of the complex can be split into a northern part where most pegmatite occurs in a single 25-30 m thick dyke and a southern part where this dyke splits into upper and lower pegmatites that then remerge 450 m further south. The width of the Fi Main corridor ranges from 25-75 m where it is dominated by a single dyke and between 75-150 m where it is split into two or more dykes. The two holes reported here were both drilled at the north end of the complex.

YLP-0250 was drilled to test the Fi Main corridor at approximately 10-125 m below the surface and 100 m due north of previously released YLP-0233 (no significant result). Over a 159 m interval, drilling intersected 11 pegmatite dykes with widths between 1 to 9 m that total to a cumulative pegmatite width of 46 m. Assays all returned ≤0.3% Li2O (Table 1 & 2, Figure 10).

YLP-0255 was drilled 50 m north of YLP-0250 to provide a similar test of the Fi Main corridor between 10-100 m below the surface. Drilling intersected 35 m of pegmatite spread over eight dykes and 101 m of drill core, with all assays returning ≤0.2% Li2O (Table 1 & 2, Figure 10).

Individual Drill plans YK pegmatites Fi NR32 GT for May 21

Figure 10 – Plan view showing the surface expression of the Fi Main 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-0244No significant resultsEcho
YLP-0250No significant resultsFi Main
YLP-0252No significant resultsEcho
YLP-025316917560.50Echo
YLP-0255No significant resultsFi Main
YLP-0256596230.57Echo
YLP-0257No significant resultsEcho
YLP-02614730.56Ki
YLP-02636678120.82Echo
incl  697561.29
YLP-0267929310.57BIG East
and  12012330.46
and  12813680.46
YLP-0274718111Ki
incl  81461.87
YLP-02833166351.32Shorty


Drilling Progress Update

Currently, LIFT has reported results from 257 diamond drill holes (44,512 m). The Company concluded its winter drill program at the Yellowknife Lithium Project with a combined total of 286 diamond drill holes (49,548 m) completed between the summer and winter programs.

General Statements

All 12 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 HoleNAD83EastingNorthingElevation (m)Depth (m)Azimuth (°)Dip (°)Dyke
YLP-0244Zone 12N439,8266,922,14528618324049Echo
YLP-0250Zone 12N371,8346,942,27425218010045Fi Main
YLP-0252Zone 12N439,6416,922,2682887824062Echo
YLP-0253Zone 12N439,7176,922,42627719224045Echo
YLP-0255Zone 12N371,8376,942,32025315010046Fi Main
YLP-0256Zone 12N439,6226,922,3182897824053Echo
YLP-0257Zone 12N439,7716,922,23328716524053Echo
YLP-0261Zone 12N373,0776,942,9412561205745Ki
YLP-0263Zone 12N439,4756,922,64427724621554Echo
YLP-0267Zone 12N346,2936,933,47719716712170BIG East
YLP-0274Zone 12N373,0116,943,0762541596045Ki
YLP-0283Zone 12N372,9576,938,37725120012464Shorty


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 MacDonald Daniel Gordon
Chief Executive Officer Investor Relations Manager
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" in the Company's latest annual information form filed on March 27, 2024, 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.

Photos accompanying this announcement are available at:

https://www.globenewswire.com/NewsRoom/AttachmentNg/8209fa1e-d5d0-46cc-9021-6be9402e2784

https://www.globenewswire.com/NewsRoom/AttachmentNg/d4d3f3bc-9c05-431f-983c-d19ac63371c5

https://www.globenewswire.com/NewsRoom/AttachmentNg/248fa149-8726-494a-af91-d3dc5dae3c19

https://www.globenewswire.com/NewsRoom/AttachmentNg/ab725495-6de8-4e12-9663-3f6b69a2cd43

https://www.globenewswire.com/NewsRoom/AttachmentNg/ce43e990-bbb4-40c7-a5a4-79643a6701f1

https://www.globenewswire.com/NewsRoom/AttachmentNg/48910c8b-0cf5-4c0f-a234-03d78d609323

https://www.globenewswire.com/NewsRoom/AttachmentNg/cd2a1b0a-a486-4fb1-bef1-f108af80b07c

https://www.globenewswire.com/NewsRoom/AttachmentNg/e83023d7-02ff-4abe-9efb-fa6f79d4b808

https://www.globenewswire.com/NewsRoom/AttachmentNg/72e00beb-e845-4f3f-84d8-f06dce5d7808

https://www.globenewswire.com/NewsRoom/AttachmentNg/66d5b2ef-d452-4b6f-93fb-ed3b65908f77

 


FAQ

What are the assay results for the Shorty pegmatite at the Yellowknife Lithium Project?

Li-FT Power reported a significant intersection of 35 meters at 1.32% Li2O at the Shorty pegmatite.

How extensive is the high-grade mineralization at Shorty?

The high-grade mineralization at Shorty extends for a total of 400 meters on the surface.

What were the highlights from the Ki pegmatite drill results?

The Ki pegmatite drill results included an 11-meter interval at 1.16% Li2O, with a 6-meter section at 1.87% Li2O.

How many drill holes were completed in the winter drilling program at YLP?

A total of 286 diamond drill holes were completed, covering 49,548 meters.

What is the significance of the 35-meter interval at Shorty?

The 35-meter interval at 1.32% Li2O indicates substantial near-surface spodumene mineralization, enhancing the project's potential.

Were there any drill holes with no significant results in the recent YLP assay report?

Yes, some drill holes, including YLP-0252 and YLP-0250, returned no significant lithium mineralization.

Which pegmatites showed promising lithium results apart from Shorty?

Apart from Shorty, the Ki and Echo pegmatites also showed promising lithium results.

What were the assay highlights for the Echo pegmatite?

The Echo pegmatite highlights include an interval of 12 meters at 0.82% Li2O, with a 6-meter section at 1.29% Li2O.

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