Highlights:
- The Company has completed 5 weeks of fieldwork, expanding the
lithium-cesium-tantalum ("LCT") pegmatite trend on the property to
a potential strike length of >25 km open at both ends.
- A total of 837 samples have now been collected at the Project,
highlighting multiple drill targets. Assays for 219 samples are
pending receipt and analysis. Highlight results include up to 0.5%
Li2O, 1,730 ppm cesium, 120,000 ppm tantalum and 3,540
ppm rubidium.
- Geochemical results indicate the strong potential for
spodumene-bearing dykes to be present at the property.
Potassium/rubidium ratios (K/Rb), are a key tool in identifying
these types of dykes; K/Rb ratios of <30 are indicative of
rare-earth pegmatites and <20 of spodumene-subtype
pegmatites[i]. To-date, 10 pegmatites have been identified with
K/Rb ratios <30 with a low of 7.5. Values below 10 are often
associated with economic spodumene pegmatites.
- The Company intends on drilling each of the 10 target
pegmatites as part of its maiden drill program.
VANCOUVER, BC, Sept. 14, 2023 /CNW/ -- Usha Resources
Ltd. ("USHA" or the "Company") (TSXV: USHA)
(OTCQB: USHAF) (FSE: JO0), a North American mineral
acquisition and exploration company, is pleased to provide this
update on its on-going field program at the White Willow Lithium
Pegmatite Project ("White Willow" or the "Project") located 170 km
west of Thunder Bay, Ontario.
The Company has completed 5 weeks of fieldwork this season, with
data compilation complete for 618 samples. Assay highlights
include:
- Lithium oxide (Li2O) values up to 0.5%, with 76
samples containing very anomalous (>300 ppm) concentrations of
lithium, including 14 above >1,000 ppm with a sample of the host
rock which assayed 1,300 ppm indicating significant lithium-rich
fluids are present within the system.
- Cesium (Cs) values up to 1,730 ppm, with 71 samples containing
very anomalous (>100 ppm) concentrations including 10 which are
>500 ppm, indicating the samples are being collected from the
outer zone of a fertile LCT system, which is where spodumene, if
present, will be identified.
- Tantalum (ta) values up to 120,000 ppm Ta, with 82 samples
containing very anomalous (>30 ppm) concentrations including 35
which are >60 ppm, indicative of the presence of a
spodumene-bearing pegmatite.
Of note, a high-grade showing of 14.64% Ta2O5
is present at the Maple Leaf Dyke; coarse-grained tantalite is only
known to be found at one other locality in Ontario which is the North Aubrey pegmatite at
Green Technology Metals (GT1) Seymour Lake Project where GT1 has
identified a 9.9 Mt resource at 1.04% Li2O.
- Rubidium values of up to 3,540 ppm, with 94 samples
containing very anomalous (>1,000 ppm) concentrations including
24 >2,000 ppm.
Geochemical assessment also indicates the strong potential for
spodumene-bearing dykes to be present at the property. Per Selway et al., potassium/rubidium ratios
(K/Rb), are a key tool in identifying these types of dykes; K/Rb
ratios of <30 are indicative of rare-earth pegmatites and <20
of spodumene-subtype pegmatites. To-date, 10 pegmatites have been
identified with K/Rb ratios <30 with a low of 7.5. Values below
10 are often associated with economic spodumene pegmatites.
Each of these pegmatites are planned to be drilled as part of
the maiden drill program scheduled to commence in Q1 of 2024.
The Company will return to Site in October to complete
additional prospecting and mapping after which it will proceed with
geophysical surveys to outline structures prior to commencing the
drill program.
"We are thrilled with the findings from the initial programs at
White Willow," said Deepak Varshney,
CEO of Usha Resources. "As seen at Patriot Battery Metals' Corvette
Project, which has over 20 kilometres of trend, lithium pegmatite
swarms occur in clusters, each of which has the potential to become
a deposit. We now have 10 primary target areas across our 25
kilometre plus trend that include two highly evolved LCT pegmatite
swarms at Bingo and Maple Leaf. With significant ground remaining
between Bingo and Maple Leaf for further exploration and follow-up,
we intend on maximizing the remaining time in the field season
before commencing preparations for maiden winter drill program. The
findings thus far strongly validate our belief that Willow is a
flagship asset where Ontario's
next major lithium discovery will occur."
Quality Assurance/Quality Control
All collected rock samples were put in sturdy plastic bags,
tagged, and sealed at site. Sample bags were then put in rice bags
and kept securely before being sent by road transport or delivered
by the crew supervisor to either AGAT Laboratories Ltd. or
Activation Laboratories in Thunder Bay,
Ontario. All samples are analyzed with Four-Acid
Digestion/Combined ICP-AES/MS package (49 elements). The QA/QC
protocol included the insertion and monitoring of appropriate
reference materials, in this case high concentration and low
concentration certified OREAS and CDN lithium standards to validate
the accuracy and precision of the assay results.
Qualified person
The technical content of this news release has been reviewed and
approved by Mr. Andrew Tims, P.Geo.,
a qualified person as defined by National Instrument 43-101.
About Usha Resources Ltd.
Usha Resources Ltd. is a North American mineral acquisition and
exploration company focused on the development of quality lithium
metal properties that are drill-ready with high-upside and
expansion potential. Based in Vancouver,
BC, Usha's portfolio of strategic properties provides
target-rich diversification and includes Jackpot Lake, a lithium
brine project in Nevada and White
Willow, a lithium pegmatite project in Ontario that is the flagship among its growing
portfolio of hard-rock lithium assets. Usha trades on the TSX
Venture Exchange under the symbol USHA, the OTCQB Exchange under
the symbol USHAF and the Frankfurt Stock Exchange under the symbol
JO0.
USHA RESOURCES LTD.
For more information, please call Tyler
Muir, Investor Relations, at 1-888-772-2452, email
tmuir@usharesources.com, or visit www.usharesources.com.
Neither TSX Venture Exchange nor its Regulation Services
Provider (as that term is defined in policies of the TSX Venture
Exchange) accepts responsibility for the adequacy or accuracy of
this release.
Forward-looking statements:
This news release may include "forward-looking information"
under applicable Canadian securities legislation. Such
forward-looking information reflects management's current beliefs
and are based on a number of estimates and/or assumptions made by
and information currently available to the Company that, while
considered reasonable, are subject to known and unknown risks,
uncertainties, and other factors that may cause the actual results
and future events to differ materially from those expressed or
implied by such forward-looking information. Readers are cautioned
that such forward-looking information are neither promises nor
guarantees and are subject to known and unknown risks and
uncertainties including, but not limited to, general business,
economic, competitive, political and social uncertainties,
uncertain and volatile equity and capital markets, lack of
available capital, actual results of exploration activities,
environmental risks, future prices of base and other metals,
operating risks, accidents, labour issues, delays in obtaining
governmental approvals and permits, and other risks in the mining
industry.
The Company is presently an exploration stage company.
Exploration is highly speculative in nature, involves many risks,
requires substantial expenditures, and may not result in the
discovery of mineral deposits that can be mined profitably.
Furthermore, the Company currently has no reserves on any of its
properties. As a result, there can be no assurance that such
forward-looking statements will prove to be accurate, and actual
results and future events could differ materially from those
anticipated in such statements.
[i] Selway, J. et al. 2005. A
Review of Rare-Element (Li-Cs-Ta) Pegmatite Exploration Techniques
for the Superior Province, Canada,
and Large Worldwide Tantalum Deposits. Exploration and Mining
Geology, Vol. 14, Nos. 1-4, pp. 1-30.
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SOURCE Usha Resources Ltd.