New Energy Metals Announces Option Agreement for Atikokan Lithium Property and Amends Troitsa Agreement
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New Energy Metals Announces Option Agreement for Atikokan Lithium
Property and Amends Troitsa Agreement
Vancouver, British Columbia, August 14, 2023 New Energy Metals Corp. (TSXV: ENRG) (OTCQB:
NRGYF) (“New Energy” or the “Company “) is pleased to announce that it has entered into an option
agreement (the " Agreement") dated July 28, 2023, to acquire a 100% interest in the highly
prospective Atikokan Lithium Property (the " Property"). The Property consists of 4 mining claims
comprising 3,788 hectares and is located approximately 12 km east of Atikokan, Ontario (Figure 1).
Figure 1. Regional location of the Atikokan lithium property.
The claims straddle the contact between a peraluminous S- type muscovite -bearing gran ite and
metasediments within the Quetico subprovince (Figure 2). The Quetico -Marmion subprovincial
boundary lies just 4 km north of the Property. Numerous lithium deposits of northwestern Ontario
occur proximal to a subprovincial boundary (Breaks et al., 2 003). Historically, the Atikokan area has
documented strongly anomalous lake sediment results in Li, Rb, Cs, Ga and Sn (Jackson, 2001).
Muscovite-bearing pegmatite dykes and small pegmatitc granite masses are widely exposed along
Highway 11 between Nym Lake Road junction and west to Niobe Lake (McIlwaine and Larsen 1981a,
1981b). In 2003, Breaks et al., took 16 bulk rock samples along Highway 11 largely within the
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Property boundary (Figure 3). Bulk rock chemistry showed a significant number of anomalous
lithium values. Lithium ranged from 11 to 164 ppm with a mean content of 72 ppm, however, 25%
and 60% of the data, respectively, exceeded 100 ppm and 50 ppm. Taylor (1964) states that lithium
values exceeding 100 ppm indicate extreme fractionation.
The Gilbe rt Lake rare -element mineral occurrence, sample 01 -JBS-78-07 within the Property
boundary was the most evolved pegmatitic rock encountered by the survey. This beryl -type
pegmatite contains maximum levels in this area for most rare-elements: Be (18 ppm), Cs (80 ppm),
Li (99 ppm), Rb (524 ppm), Sn (177 ppm), Ta (20 ppm), Nb (42 ppm) and Ga (81 ppm) (Breaks et al.,
2003).
Figure 2. Regional geology of the Atikokan lithium property.
Figure 3. Bulk sample locations by Breaks et al., 2003.
For the rare alkali metals, cesium was significantly enriched 7 to 25 times above its mean crustal
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abundance for 80% of the data population and varied from 3.9 to 80 ppm. Many values exceeded 15
ppm, a level considered by Černý and Meintzer (1988) to indicate significant fractionation in granitic
systems. Rubidium had a range of 5 to 534 ppm and mean content of 270 ppm.
In essence, Breaks et al., 2003 summed up their reconnaissance prospecting and mapping with:
“The anomalous Li, Rb, Cs, Sn and Ga documented in the bedrock by this survey corroborate the
earlier lake sediment geochemistry work of Jackson (2001). Exploration for rare -element
mineralization in the area should therefore focus on the numerous lake sediment anomalies for
these metals in the general area as th ere is a close correlation with bedrock chemical data at least
in the Nym-Niobe lakes area. The discovery of columbite-tantalite group minerals and beryl by this
survey gives strong indications that, with careful prospecting, further rare-element minerals may be
discovered. The presence of elevated Ta contents in bulk muscovite at localities 01-FWB-126 and 01-
JBS-81 suggests that they should be investigated further for possible tantalum mineralization”.
Under the terms of the Agreement, New Energy has the right to acquire a 100% interest in the
Property by making aggregate cash payments of $66,000 over a period of two years. The optionors
will retain a 3% net smelter returns royalty.
The technical information contained in this news release has been reviewed and approved by Mike
Kilbourne, P . Geo., a Qualified Person as defined in National Instrument 43 -101 - Standards of
Disclosure for Mineral Projects.
The acquisition is an arm's length transaction and qualifies as an “Exempt Transaction” pursuant to
the policies of the TSX Venture Exchange.
The Company also wishes to announce that it has amended the terms of the Troitsa option
agreement (the “Troitsa Agreement”) pursuant to which the Company will issue 900,000 shares (the
“Shares”) of the Company to the optionor in lieu of the cash payment of $ 45,000 due in July 2023.
The Company or its assignees will have the right of first refusal to purchase the Shares. All other
terms of the Troitsa Agreement remain the same.
ON BEHALF OF THE BOARD OF DIRECTORS,
New Energy Metals Corp.
Rishi Kwatra
CEO & Director
#610 – 700 West Pender Street
Vancouver, BC V6C 1G8 Canada
Tel: 604-669-9788
www.new-enrg.com
References
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1. Breaks, F.W., Selway, J.B. and Tindle, A.G. 2003. Fertile peraluminous granites and related
rare-element mineralization in pegmatites, Superior Province, northwest and northeast Ontario:
Operation Treasure Hunt; Ontario Geological Survey, Open File Report 6099, 179p.
About New Energy Metals Corp.
New Energy is a Canadian -based resource company listed on the TSX Venture Exchange under the
symbol ENRG. The Company has an option to purchase a 100-per-cent interest in the Roslyn lithium
property, covering 5,100 hectares located 20 kilometers southeast of the Georgia Lake pegmatite
field and 35 kilometers southeast of where Rock Tech Lithium just published a preliminary economic
assessment supporting the indicated mineral resource of 10.6 Mt (million tons) grading 0.88 per cent
lithium oxide and an inferred mineral resource of 4.2 Mt grading 1.0 per cent Li2O. The Company
also has an option to purchase a 100 -per-cent interest in the Troitsa co pper property covering
approximately 7,000 hectares located in the Omineca mining division of British Columbia.
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the
policies of the TSX Venture Exchange) acc epts responsibility for the adequacy or accuracy of this
release.
Cautionary Statement on Forward Looking Information
Certain statements made, and information contained herein may constitute “forward looking
information” and “forward looking statements” within the meaning of applicable Canadian
and United States securities legislation. These statements and information are based on facts
currently available to the Company and there is no assurance that actual results will meet
management’s expectations. Forward-looking statements and information may be identified by such
terms as “anticipates”, “believes”, “targets”, “estim ates”, “plans”, “expects”, “may”, “will”,
“speculates”, “could” or “would”.
All of the forward -looking statements made in this document are qualified by these cautionary
statements. Although the Company has attempted to identify important factors that could cause
actual results to differ materially from those contained in forward-looking information, there may be
other factors that cause results not to be as anticipated, estimated, forecast or intended and readers
are cautioned that the foregoing list is not exhaustive of all factors and assumptions which may have
been used. Should one or more of these risks and uncertainties materialize, or should underlying
assumptions prove incorrect, actual results may vary materially from those described in forward-
looking information. Accordingly, there can be no assurance that forward- looking information will
prove to be accurate and forward- looking information is not a guarantee of future performance.
Readers are advised not to place undue reliance on forward- looking information. The forward-
looking information contained herein speaks only as of the date of this document. The Company
disclaims any intention or obligation to update or revise forward –looking information or to explain
any material difference between such and subsequent actual events, except as required by applicable
law.