LIFT Intersects 23 m at 1.40% Li2O at its Fi Main pegmatite, Yellowknife Lithium Project, NWT
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VANCOUVER, British Columbia, Jan. 23, 2024 (GLOBE NEWSWIRE) -- 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 Main, 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-0148: 23 m at
1.40% Li2O, (Fi Main) - YLP-0182: 11 m at
1.38% Li2O, (Nite) - YLP-0145: 10 m at
1.28% Li2O, (Nite)
and: 3 m at1.26% Li2O - YLP-0149: 5 m at
1.04% Li2O, (Nite)
and: 1 m at1.04% Li2O
and: 10 m at0.78% Li2O
including: 5 m at1.15% Li2O
Discussion of Results
This week’s drill results are for eight holes drilled on four separate pegmatite complexes, including Fi Main (N = 1), Nite (N = 3), BIG West (N = 2), and Ki (N = 2). 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.
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.
Fi Main Pegmatite
The Fi Main pegmatite comprises a 10-100 m wide corridor of 1-5 dykes that dip between 70°-85° to the west-northwest and extends for at least 1.5 km on surface.
YLP-0148 tested the Fi Main pegmatite approximately 300 m from its northern mapped extent, 50 m vertically beneath the surface, and 250 m up-dip from YLP-0020 (
Figure 2 – Plan view showing the surface expression of the Fi Main pegmatite with diamond drill holes reported in this press release.
Figure 3 – Cross-section illustrating YLP-0148 with results as shown in the Fi Main pegmatite dyke with a 23 m interval of
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° degrees to the east.
YLP-0145 was designed to test the Nite pegmatite approximately 500 m from its northern mapped extent, <25 m vertically beneath the surface, and 50 m up-dip from YLP-0149 (see next paragraph). Drilling intersected three pegmatite dykes from the base of overburden (B-OVB) to 40 m core depth, ranging from 2-13 m in width for cumulative pegmatite width of 18 m. The widest dyke returned an assay composite of
YLP-0149 was designed to test the Nite pegmatite on the same section as YLP-0145 but at 50 m further downdip. Drilling intersected four pegmatite dykes ranging from 1-11 m in width for cumulative pegmatite width of 27 m over 43 m of core length. The three widest dykes, from upper- to lower-most, returned assay composites of
YLP-0182 was designed to test the Nite pegmatite approximately 600 m from its southern mapped extent, 250 m vertically beneath the surface, and 200 m down-dip of YLP-0142 (
Figure 4 – Plan view showing the surface expression of the Nite pegmatite with diamond drill hole reported in this press release.
Figure 5 – Cross-section of YLP-0182 which intersected the Nite pegmatite dyke with a 11 m interval of
Figure 6 – Cross-section of YLP-0145 which intersected the Nite pegmatite dyke with a 10 m interval of
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 approximately 50-100 m apart in the north half and just under 150 m apart in the southern part. To facilitate description, these dykes are here referred to as the east bounding (EB) and west bounding (WB) dykes.
YLP-0151 tested the BIG West EB dyke approximately 150 m from its southern mapped extent, 150 m vertically below the surface, and 100 m down-dip of YLP-0146 (
YLP-0153 was designed to test the WB dyke approximately 350 m from its southern mapped extent and <25 m vertically beneath the surface, as well as 50 m up-dip from YLP-0135 (
Figure 7 – Plan view showing the surface expression of the BIG West pegmatite with diamond drill holes reported in this press release.
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-0155 tested the Ki pegmatite approximately 300 m from its southern mapped extent and 100 m vertically beneath the surface, as well as 50 m down-dip of YLP-0096 (
YLP-0161 tested the Ki pegmatite approximately 400 m from its southern mapped extents, 150 m vertically beneath the surface, and 100 m down-dip of YLP-0110 (
Figure 8 – Plan view showing the surface expression of the Ki 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-0145 | 1 | 4 | 3 | 1.26 | Nite |
and | 20 | 30 | 10 | 1.28 | Nite |
YLP-0148 | 72 | 95 | 23 | 1.40 | Fi Main |
YLP-0149 | 65 | 70 | 5 | 1.04 | Nite |
and | 80 | 81 | 1 | 1.04 | Nite |
and | 85 | 95 | 10 | 0.78 | Nite |
inc | 89 | 94 | 5 | 1.15 | Nite |
YLP-0151 | 178 | 179 | 1 | 0.62 | BIG West |
YLP-0153 | 3 | 12 | 9 | 0.99 | BIG West |
YLP-0155 | No significant results | Ki | |||
YLP-0161 | No significant results | Ki | |||
YLP-0182 | 302 | 313 | 11 | 1.38 | Nite |
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 156 out of 198 diamond drill holes (27,493 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
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-0145 | Zone 11 | 647,535 | 6,936,519 | 207 | 300 | 45 | 57 | Nite |
YLP-0148 | Zone 12 | 371,785 | 6,941,865 | 251 | 91 | 50 | 114 | Fi Main |
YLP-0149 | Zone 11 | 647,591 | 6,936,490 | 208 | 300 | 46 | 123 | Nite |
YLP-0151 | Zone 11 | 653,932 | 6,932,852 | 202 | 298 | 45 | 230 | BIG West |
YLP-0153 | Zone 11 | 653,721 | 6,933,079 | 209 | 118 | 45 | 32 | BIG West |
YLP-0155 | Zone 12 | 373,101 | 6,942,606 | 254 | 57 | 57 | 252 | Ki |
YLP-0161 | Zone 12 | 372,944 | 6,942,620 | 256 | 55 | 58 | 325 | Ki |
YLP-0182 | Zone 11 | 647,623 | 6,936,125 | 215 | 298 | 53 | 351 | Nite |
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
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 Chief Executive Officer Tel: + 1.604.609.6185 Email: info@li-ft.com Website: www.li-ft.com | Daniel Gordon Investor Relations Tel: +1.604.609.6185 Email: investors@li-ft.com |
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FAQ
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