VANCOUVER, BC, April 24,
2023 /CNW/ - Argentina Lithium & Energy
Corp. (TSXV: LIT) (FSE: OAY3) (OTC: PNXLF), ("Argentina
Lithium" or the "Company") reports continued positive lithium
brine results at its Rincon West Project in Salta Province, Argentina, including a 178 m* section with results ranging from 241 to
340 mg/l lithium (*no sample was collected from 30 m of this interval) from the seventh diamond
drill hole of the current program.

"These new results demonstrate the continuity of concentrated
lithium brines within our exploration area and expands the area
known to host lithium brines to the northwest. We have been pleased
by the extensive vertical column of concentrated brines intersected
to date in the core of our basin. The drill program has confirmed
the original geophysical interpretation for conductive brine
aquifers very well, providing confidence in the potential for
future drilling on the extensive untested portions of the
geophysical anomaly to continue to potentially extend our zone of
lithium-rich brines." stated Miles
Rideout, V.P. of Exploration.
The results of the brine analyses for holes seven and eight are
shown in Table 1, as well as the type of sample collected, and the
respective intervals from which brine was recovered. The ninth and
final hole of the program was recently completed and laboratory
analytical results are pending.
Rincon West Project and Program
Details
The Rincon West Project, located west and north of Rio Tinto's
adjacent Rincon Project, covers 3742.8 hectares of the salar
basin. Figure 1 presents a map of the Rincon West
property showing the positions of the nine permitted and completed
exploration holes from this program (see News Releases dated
July 13, 2022, October 3, 2022, October
25, 2022 and January 26,
2023). The map in Figure 1 displays the drill locations
overlaid on the conductive zones delineated with TEM geophysics
(see May 2, 2022 News Release; Note:
the easternmost property extension was acquired after the
completion of the TEM survey and therefore shows no geophysics
results).
Drilling was carried out by Salta-based AGV Falcon Drilling SRL,
under the supervision of Argentina Lithium's geologists. Drill
holes RW-DDH-007 and RW-DDH-008 were executed with diamond
drilling (HQ-diameter), permitting the extraction of core samples
of the salar basin formations and recovery of brine samples where
possible. Argentina Lithium's preferred method for brine sampling
deploys a 'single packer' sampling unit during drilling. The packer
sampling method allows the recovery of brine samples at specific
depths while sealing the hole at the top and bottom of the
interval. For single packer sampling, an inflatable seal closes the
top of the interval; the lower limit of drilling represents the
bottom of the interval. In certain instances, double packer
sampling is conducted following the completion of drilling. In this
case, inflatable seals are employed to close both the top and
bottom of the sample interval. The maximum span of double packer
sampling is limited to less than 4 m
by the height of the drill mast and other equipment
limitations.
Table 1: Interval data and results of brines analyses
for lithium, potassium, and magnesium for drill holes
RW-DDH-007 and RW-DDH-008
Sample interval
(m)
|
Sample
Method
|
Li
|
K
|
Mg
|
Density
|
From
|
To
|
Thickness
|
|
(mg/litre)
|
(g/ml)
|
RW-DDH-007
|
|
|
|
113
|
143
|
30
|
Single
packer
|
197
|
3591
|
1910
|
1.121
|
143
|
167
|
24
|
Single
packer
|
278
|
5475
|
2378
|
1.171
|
167
|
191
|
24
|
Single
packer
|
286
|
5691
|
2415
|
1.171
|
191
|
212
|
21
|
Single
packer
|
297
|
5793
|
2529
|
1.176
|
212
|
230
|
18
|
Single
packer
|
285
|
5486
|
2470
|
1.170
|
230
|
248
|
18
|
Single
packer
|
271
|
5174
|
2351
|
1.160
|
266
|
284
|
18
|
Single
packer
|
241
|
4446
|
2147
|
1.139
|
296
|
321
|
25
|
Single
packer
|
340
|
6460
|
2863
|
1.192
|
141
|
144
|
3
|
Double
packer
|
291
|
5438
|
2551
|
1.166
|
156
|
159
|
3
|
Double
packer
|
264
|
4950
|
2297
|
1.153
|
168
|
171
|
3
|
Double
packer
|
285
|
5314
|
2511
|
1.164
|
180
|
183
|
3
|
Double
packer
|
280
|
5217
|
2419
|
1.158
|
RW-DDH-008
|
|
|
|
80
|
98
|
18
|
Single
packer
|
<10
|
<20
|
<10
|
1.001
|
98
|
113
|
15
|
Single
packer
|
<10
|
42
|
67
|
1.002
|
110
|
125
|
15
|
Single
packer
|
57
|
943
|
1046
|
1.040
|
140
|
155
|
15
|
Single
packer
|
312
|
5629
|
2861
|
1.180
|
182
|
197
|
15
|
Single
packer
|
228
|
4044
|
2042
|
1.136
|
197
|
212
|
15
|
Single
packer
|
355
|
6148
|
3088
|
1.195
|
*Both drill holes were
inclined vertically; the salar strata are believed to be flat lying
resulting in reported intervals approximating true
thickness.
|
Table 2:
Collar and maximum depth information for RW-DDH-007 and
RW-DDH-008
|
Hole
ID
|
East
|
North
|
Elevation
|
Azimuth
|
Dip
|
Depth
|
|
UTM Zone 19S
(WGS84)
|
(m)
|
(deg.)
|
(deg.)
|
(m)
|
RW-DDH-007
|
681453
|
7337379
|
3775
|
n/a
|
90
|
347.0
|
RW-DDH-008
|
680688
|
7337736
|
3781
|
n/a
|
90
|
323.0
|
Observations regarding
RW-DDH-007
RW-DDH-007 is an in-fill hole in the south-central portion of
the basin. From near surface to 66 m
depth, sandy units were crossed with gravel and clay beds. Sulphate
minerals appear in the sedimentary sequence below 66 m, with particularly high concentration
between 90 and 116 m depths.
Fine-to-medium sandy units extended from 116 to 191 m, with layers of clay, sulphates and fine
gravels observed infrequently. Basement clasts were also observed
sporadically at some levels. From 191 to 215
m depth, a unit of coarse-to-medium sands was
intersected. Ignimbrites with little fracturing were
intersected between 215 and 285 m
depths. From 285 m to the bottom of
the hole, what are interpreted as basement units with varying
degrees of alteration and silicification were intersected. The hole
was terminated at 347 m depth in
argillic-altered granite.
Observations regarding
RW-DDH-008
RW-DDH-008 extends drilling to the northwest and infills an
undrilled area between holes RW-DDH-005 and 006. Gravels and
sands were drilled in the top 26 m of
this hole, underlain by 6 m of
weakly-cemented volcanic tuff. Sandy units resumed at 32 m, initially with a large amount of organic
material, and with sulphates beginning at 37
m depth. A silt layer with clay was crossed between 40 and
62 m. Fine sands with coarse gravel
layers were intersected between 62 and 83
m, extending to 86 m with
poorly consolidated sands. There follow 5
m of sands in a clay matrix, and from 91 to 122 m, coarse-to-medium sands containing basement
clasts. From 122 to 182 m, another
coarse-to-medium sandy unit was crossed exhibiting ignimbrite
clasts and very infrequent clay layers. The hole crossed ignimbrite
with little fracturing between 182 and 277
m depth. The underlying transition showed 1.5 m of breccia with angular basement clasts,
followed by quartzite basement. The uppermost 30 m of basement displays fractures filled with
pyrite, hematite and chlorite. The drill was stopped at
323 m in quartzite basement with
little fracturing.
All core samples recovered by drilling were retained for
geologic logging. An extensive selection of samples has been sent
for brine recovery testing at an independent laboratory. This
analysis remains pending.
Analyses and QA/QC
Samples of brine were submitted for analysis to Alex Stewart
International Argentina S.A. ("Alex Stewart"), the local subsidiary
of Alex Stewart International, an ISO 9001:2008 certified
laboratory, with ISO 17025:2005 certification for the analysis of
lithium, potassium and other elements. Alex
Stewart employed Inductively Coupled Plasma Optical Emission
Spectrometry ("ICP-OES") as the analytical technique for the
primary constituents of interest, including boron, calcium,
potassium, lithium, and magnesium. Measurements in the field
included pH, electrical conductivity, temperature and density. The
quality of sample analytical results was controlled and assessed
with a protocol of blank, duplicate and reference standard samples
included within the sample sequence. For the holes RW-DDH-007 and
008 reported herein, the blank (2) and duplicate (2) samples
reported within the acceptable range. A single
low-grade and either a medium-grade or high-grade reference
standard sample was included within the submitted samples for each
hole. The low-grade reference standard analyses were above 3
standard deviations (SD) with between 2.0 and 8.6 relative percent
difference (RPD) from the best value; the medium grade reference
standard inserted into the hole RW-DDH-007 sample sequence was
within 2 SD below the best value with 0.75 RPD; the high-grade
reference standard inserted into the hole RW-DDH-008 sample
sequence returned less than 3 SD below the best value with a 2.46
RPD.
Qualified Person
David Terry, Ph.D., P.Geo. is the
Company's Qualified Person as defined in National Instrument
43-101. Dr. Terry is responsible for oversight of the Company's
early-stage exploration at the Rincon West property. The
disclosure in this news release has been reviewed and approved by
Dr. Terry.
About Argentina Lithium
Argentina Lithium & Energy Corp is focused on acquiring high
quality lithium projects in Argentina and advancing them toward production
in order to meet the growing global demand from the battery sector.
The management group has a long history of success in the resource
sector of Argentina and has
assembled a first-rate team of experts to acquire and advance the
best lithium properties in the "Lithium Triangle". The Company is a
member of the Grosso Group, a resource management group that has
pioneered exploration in Argentina
since 1993.
ON BEHALF OF THE BOARD
"Nikolaos Cacos"
_______________________________
Nikolaos Cacos, President, CEO and
Director
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.
This news release may contain forward-looking statements.
Forward-looking statements address future events and
conditions and therefore involve inherent risks and uncertainties.
All statements, other than statements of historical fact, that
address activities, events or developments the Company believes,
expects or anticipates will or may occur in the future, including,
without limitation, statements about the Company's plans for its
mineral properties; the Company's business strategy, plans and
outlooks; the future financial or operating performance of the
Company; and future exploration and operating plans are
forward-looking statements.
Forward-looking statements are subject to a number of risks
and uncertainties that may cause the actual results of the Company
to differ materially from those discussed in the forward-looking
statements and, even if such actual results are realized or
substantially realized, there can be no assurance that they will
have the expected consequences to, or effects on, the Company.
Factors that could cause actual results or events to differ
materially from current expectations include, among other things:
the impact of COVID-19; risks and uncertainties related to the
ability to obtain, amend, or maintain licenses, permits, or surface
rights; risks associated with technical difficulties in connection
with mining activities; and the possibility that future
exploration, development or mining results will not be consistent
with the Company's expectations. Actual results may
differ materially from those currently anticipated in such
statements. Readers are encouraged to refer to the Company's public
disclosure documents for a more detailed discussion of factors that
may impact expected future results. The Company undertakes no
obligation to publicly update or revise any forward-looking
statements, unless required pursuant to applicable laws. We advise
U.S. investors that the SEC's mining guidelines strictly prohibit
information of this type in documents filed with the SEC. U.S.
investors are cautioned that mineral deposits on adjacent
properties are not indicative of mineral deposits on our
properties.
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