Amended Announcement – Patriot Makes New Discovery at the Corvette Property as it Intercepts 100 m of Spodumene-Bearing Pegmatite at CV9, Quebec, Canada
Pa
triot Battery Metals Inc.
Suite 700 - 838 W. Hastings Street, Vancouver, BC, Canada, V6C 0A6
www.patriotbatterymetals.com TSX-V: PMET / ASX: PMT / OTC: PMETF / FSE: R9GA
Amended Announcement – Patriot Makes New Discovery at the
Corvette Property as it Intercepts 100 m of Spodumene-Bearing
Pegmatite at CV9, Quebec, Canada
November 23, 2023 – Vancouver, BC, Canada November 24, 2023 – Sydney, Australia
Pat
riot Battery Metals Inc. (the “Company” or “Patriot”) (TSX -V: PMET) (ASX: PMT)
(OTCQX: PMETF) (FSE: R9GA) provides an updated announcement to the announcement
dated 21 November 2023 (Vancouver, BC, Canada) and 22 November 2023 (Sydney, Australia),
which now includes a summary table of additional information (Table A) to intervals visually
observed. Table A includes an estimation of the relative abundance of spodumene content present
within the drillholes.
This visual percentage estimate of spodumene was requested by the ASX , to comply with ASX
specific regulations , and is provided to satisfy ASX listing requirements. However, visual
estimates are subjective and, in this instance, the intent was to identify the presence of spodumene,
not the grade. The company will provide details of grade when they become available.
The amended announcement follows.
Patriot Makes New Discovery at the Corvette Property as it
Intercepts 100 m of Spodumene-Bearing Pegmatite at CV9, Quebec,
Canada
November 21, 2023 – Vancouver, BC, Canada November 22, 2023 – Sydney, Australia
Highlights
• Drill hole CV23-345 hits approximately 100 m of near-continuous spodumene-bearing
pegmatite at CV9.
• Three (3) drill holes have returned continuous pegmatite intersections of 60+ m.
• Patriot has defined a p egmatite strike length of approximately 450 m by drilling and
outcrop at CV9, which remains open.
• CV9 is located approximately 14 km west of the CV5 mineral resource.
• Preliminary geological modelling indicates the CV9 Pegmatite significantly thickens to
at least 80 m width at one location and remains open in multiple directions.
• The magnitude of this variably mineralized pegmatite blow -out is significant, sharing
similarities to those present at the CV5 Pegmatite in terms of depth and scale.
• Eighteen (18) core holes (~4,000 m) have been completed in the inaugural drill program at
the CV9 Pegmatite – sample assays are pending.
• While it is early stage, the work done to date has resulted in an improvement in the
understanding of the CV9 Pegmatite as the program went on, with a number of high priority
targets now identified.
Darren L. Smith, Company Vice President of Exploration, comments: “This is a very strong start
to the drill exploration at the CV9 Pegmatite. Although no core assays have been received yet, the
presence of spodumene and the length of pegmatite encountered in multiple holes, highlighted by
an approximate 100 m near -continuous spodumene-bearing hit in the final hole of the program,
are very positive in terms of potential of this pegmatite to hold significant scale.”
Patriot Battery Metals Inc. (the “Company” or “Patriot”) ( TSX-V: PMET) (ASX: PMT)
(OTCQX: PMETF) (FSE: R9GA) is pleased to announce preliminary results of its inaugural
drill program at the CV9 Spodumene Pegmatite at its wholly owned Corvette Property (the
“Property” or “Project”), located in the Eeyou Istchee James Bay region of Quebec . The CV9
Spodumene Pegmatite is located approximately 14 km west of the CV5 Spodumene Pegmatite
(109.2 Mt at 1.42% Li 2O inferred1), 9.5 km west-northwest of the CV13 Spodumene Pegmatite ,
and 11 km south of the Trans-Taiga Road and powerline infrastructure.
A total of eighteen (18) holes , for approximately 4,000 m of NQ cor ing, were completed this
summer-fall in the inaugural drill program at the CV9 Spodumene Pegmatite (Figure 1 and Figure
2). The Company is pleased to report that wide intervals of pegmatite, dominantly spodumene-
bearing, have been returned from multiple drill holes at CV9, including:
• 100 m in drill hole CV23-345 (includes ~1 m of non-pegmatite dilution),
• 76 m in drill hole CV23-315,
• 70 m and 27 m in drill hole CV23-333,
• 37 m in drill hole CV23-326, and
• 23 m in drill hole CV23-304
Table A: Spodumene-bearing pegmatite with respect to intervals for drill holes CV23 -304, 315,
326, 333, and 345 as listed above.
Visual estimates of mineral abundance should never be considered a proxy or substitute for
laboratory analyses where concentrations or grades are the factor of principal economic interest.
Visual estimates also potentially provide no information regarding impurities or deleterious
physical properties relevant to valuations. The pegmatite drill logs for all eighteen (18) holes will
be formally and fully logged over the next two weeks and core sample assays for the entire
pegmatite interval are anticipated to be received from the lab, and reported by the Company, in
late Q1 2024.
Although the Company does not comment on the grade of the pegmatite intervals reported, several
drill holes are noted as having pegmatite intervals that are spodumene -bearing based on
preliminary geological logging. Readers are cautioned that the potential content and quantities of
spodumene are conceptual in nature; there has been insufficient exploration by the Company or its
qualified person at the Property to define a mineral resource; and it is uncertain whether further
exploration will result in these targets being delineated as a mineral resource. Spodumene-bearing
pegmatite refers to the visually identified presence of the mineral spodumene at a minimum trace
level (i.e., 0.1 to 5%), within the respective interval, which occurs as discrete mineral crystals of
varying size, abundance, and orientation hosted within a quartz-feldspar pegmatite with accessory
muscovite and occasional tourmaline. For the relevant drill holes, the abundance of spodumene
may vary widely over the interval and, where present, has been preliminarily logged at a trace level
or higher. However, the Company notes these are preliminary logs, which are primarily used for
an initial assessment of the drill hole to guide the immediate future drill targetting. Preliminary
estimates of s podumene content may change on final logging; however, the determination as to
the presence of spodumene within an interval is unlikely to change. The Company makes no
assertions as to spodumene contents beyond spodumene being identified as present within the
interval (i.e., greater than 0.1 – 5% ) and therefore should not be relied upon as an indication of
grade. The presence of spodumene is a determining factor in indicating if the pegmatite is
Hold ID From
(m)
To
(
m)
Interval
(m)
Preliminary Estimated
Spodumene Content
CV23-304 39.3 63.0 23. 7 0.1 - 5%
CV23-315 155.9 171.7 15.8 0.1 - 5%
CV23-326 14.8 27.3 12.5 0.1 - 5%
74.6 101.7 27.1 0.1 - 5%
109.5 179.6 70.1 0.1 - 5%
CV23-345 128.5 229.4 100.9 0.1 - 5%
CV23-333
spodumene-bearing and, in turn, its presence is a positive indicator of potential for the CV9
Pegmatite target.
Figure 1: Drill holes completed at the CV9 Spodumene Pegmatite.
Preliminary logs for all pegmatite drill intercepts >2 m are presented in Table 1, and drill hole
attributes in Table 2. Drill core f rom holes completed at the CV9 Pegmatite is currently being
processed at site and no core sample assays have been received yet.
Table 1: Preliminary pegmatite logs for drill holes completed at the CV9 Spodumene Pegmatite
A primary objective of the inaugural drill program at CV9 wa s to determine the geometry and
orientation of the pegmatite system. Therefore, drill holes were completed at a variety of
orientations from multiple collar locations (Figure 1) with results consistently improving over the
course of the program as understanding of the pegmatite geometry improved. The last eight (8)
holes all returned continuous core-length pegmatite intercepts >10 m, including three (3)
intersections of 60+ m (see Figure 1 and Table 1).
The CV9 Pegmatite is currently interpreted to be a single principal dyke, which outcrops at surface,
has a steep northerly dip , and is moderately plunging to the east -southeast. A strike length of
approximately 450 m has been defined to date by drilling and outcrop, which remains open
(Figure 1). The width of the dyke is variable; however, preliminary geological modelling indicates
the CV9 Pegmatite significantly thickens to at least 80 m width at one location and remains
open in multiple directions. The thickening is delineated by three (3), wide, variably mineralized
spodumene-bearing pegmatite intersections at different orientations – 70 m (CV23 -333), 76 m
(CV23-315), and 100 m (CV23-345), all core length. The magnitude of this variably mineralized
pegmatite blow-out is significant, sharing similarities to those present at the CV5 Pegmatite in
terms of depth and scale. This is a very positive observation for this early phase of drill exploration
at the CV9 Pegmatite and suggests a strong potential for significant scale to be present.
Hole ID From
(m)
To
(m)
Interval
(m)
Li2O
(%)
Ta2O5
(ppm) Hole ID From
(m)
To
(m)
Interval
(m)
Li2O
(%)
Ta2O5
(ppm)
CV23-247 No pegmatite intersected CV23-310 63.4 75.4 12.0 Assays pending
CV23-254 No pegmatite intersected 77.0 94.9 17.9 Assays pending
CV23-261 51.1 58.0 6.9 Assays pending CV23-315 155.9 171.7 15.8 Assays pending
CV23-264 48.1 51.3 3.2 Assays pending 186.1 262.2 76.1 Assays pending
97.6 99.5 2.0 Assays pending CV23-326 14.8 27.3 12.5 Assays pending
CV23-267 31.9 34.9 3.0 Assays pending 30.8 68.6 37.8 Assays pending
35.4 38.2 2.8 Assays pending 79.1 82.0 2.9 Assays pending
41.3 43.5 2.3 Assays pending CV23-333 48.8 53.9 5.1 Assays pending
58.7 63.4 4.7 Assays pending 58.2 60.2 2.1 Assays pending
68.3 84.0 15.7 Assays pending 74.6 101.7 27.1 Assays pending
87.8 94.1 6.3 Assays pending 109.5 179.6 70.1 Assays pending
CV23-275 No >2 m pegmatite intersections CV23-341 131.3 147.8 16.5 Assays pending
CV23-278 36.2 44.2 8.0 Assays pending 149.7 151.8 2.1 Assays pending
CV23-281 11.0 24.1 13.1 Assays pending 168.1 177.4 9.3 Assays pending
46.0 49.1 3.1 Assays pending CV23-345 14.3 24.3 10.0 Assays pending
CV23-284 11.6 24.9 13.4 Assays pending 81.3 88.7 7.4 Assays pending
69.5 72.2 2.7 Assays pending 128.5 164.9 36.4 Assays pending
CV23-289 12.5 21.2 8.7 Assays pending 166.0 229.4 63.4 Assays pending
61.7 63.7 2.0 Assays pending 269.5 271.9 2.4 Assays pending
CV23-296 18.6 25.5 6.9 Assays pending 315.3 324.6 9.3 Assays pending
153.7 165.0 11.3 Assays pending
186.7 190.6 3.9 Assays pending
205.2 207.5 2.3 Assays pending
CV23-304 39.3 63.0 23.7 Assays pending
(1) All intervals are core length and presented for all pegmatite
intervals >2 m; (2) Pegmatite logs for all drill holes are preliminary
and may change upon final validation.
The Company will refine the geological model for CV9 upon the receipt of assays and a follow -
up drill program will be developed to expand upon the success discussed herein.
Figure 2: Location of the CV9 Spodumene Pegmatite on the Corvette Property.
Figure 3: Spodumene mineralized outcrop at the CV9 Pegmatite (looking west-northwest).
Figure 4: Drill hole CV23-247 at the CV9 Pegmatite (looking northerly).
The 2023 summer -fall program included the inaugural drill testing of the CV9 Spodumene
Pegmatite, in addition to the continued drill delineation of the CV5 and CV13 spodumene
pegmatites. Core sample assays remain to be announced for more than 140 drill holes completed
over the program, including all 18 holes completed at CV9. Assays for CV9 drill core samples are
not expected to be received (and reported) until Q1 2024.
Core processing is continuing at site with drilling temporarily paused for the onset of winter;
drilling will resume in early January with a ramp up to ten (10) drill rigs . Core samples from a
large number of drill holes have now arrived at the laboratory with processing underway, and
shipments are now back to their regular weekly schedule. Results are anticipated to be reported in
batches per pegmatite (CV5, CV13, and CV9) as received.
Table 2: Attributes for drill holes reported herein at the CV9 Spodumene Pegmatite
1 The CV5 mineral resource estimate (109.2 Mt at 1.42% Li2O and 160 ppm Ta2O5 inferred) is reported at
a cut-off grade of 0.40% Li2O with effective date of June 25, 2023 (through drill hole CV23-190). Mineral
resources are not mineral reserves as they do not have demonstrated economic viability.
Visual estimates of mineral abundance should never be considered a proxy or substitute for
laboratory analyses where concentrations or grades are the factor of principal economic interest.
Visual estimates also potentially provide no information regarding impurities or deleterious
physical properties relevant to valuations. The pegmatite drill logs for all eighteen (18) holes will
be formally and fully logged over the next two weeks and core sample assays for the entire
pegmatite interval are anticipated to be received from the lab, and reported by the Company, in
late Q1 2024.
Although the Company does not comment on the grade of the pegmatite intervals reported, several
drill holes are noted as having pegmatite intervals that are spodumene -bearing based on
preliminary geological logging. Readers are cautioned that the potential content and quantities of
spodumene are conceptual in nature; there has been insufficient exploration by the Company or its
qualified person at the Property to define a mineral resource; and it is uncertain whether further
exploration will result in these targets being delineated as a mineral resource. Spodumene-bearing
pegmatite refers to the visually identified presence of the mineral spodumene at a minimum trace
level (i.e., 0.1 to 5%), within the respective interval, which occurs as discrete mineral crystals of
varying size, abundance, and orientation hosted within a quartz-feldspar pegmatite with accessory
muscovite and occasional tourmaline. For the relevant drill holes, the abundance of spodumene
may vary widely over the interval and, where present, has been preliminarily logged at a trace level
or higher. However, the Company notes these are preliminary logs, which are primarily used for
Hole ID Substrate Total Depth (m) Azimuth (°) Dip (°) Easting Northing Elevation (m) Core Size Cluster Comments
CV23-247 Land 143.0 160 -55 554192.9 5930116.9 400.6 NQ CV9
CV23-254 Land 200.0 250 -45 554191.4 5930116.9 400.5 NQ CV9
CV23-261 Land 183.5 0 -45 554180.2 5930038.0 403.8 NQ CV9
CV23-264 Land 206.0 0 -75 554180.1 5930037.5 403.8 NQ CV9
CV23-267 Land 186.0 60 -45 554183.5 5930037.4 403.8 NQ CV9
CV23-275 Land 197.0 0 -45 554125.9 5930056.2 405.0 NQ CV9
CV23-278 Land 152.0 60 -45 554132.2 5930058.7 404.9 NQ CV9
CV23-281 Land 209.0 255 -45 554480.0 5930084.1 402.8 NQ CV9
CV23-284 Land 155.0 165 -45 554482.6 5930081.3 403.1 NQ CV9
CV23-289 Land 215.0 290 -45 554519.4 5930044.6 401.5 NQ CV9
CV23-296 Land 279.0 235 -45 554520.4 5930042.1 401.2 NQ CV9
CV23-304 Land 230.0 160 -45 554525.3 5930043.3 401.3 NQ CV9
CV23-310 Land 230.0 0 -45 554249.2 5929997.8 398.4 NQ CV9
CV23-315 Land 308.0 80 -45 554251.7 5929995.6 398.0 NQ CV9
CV23-326 Land 239.0 160 -65 554297.2 5930042.8 401.0 NQ CV9
CV23-333 Land 287.0 0 -45 554397.0 5929909.9 382.6 NQ CV9
CV23-341 Land 212.0 40 -45 554400.0 5929900.0 375.2 NQ CV9
CV23-345 Land 374.0 255 -55 554521.6 5930050.6 402.6 NQ CV9
(1) Coordinate system NAD83 / UTM zone 18N; (2) All drill holes are diamond drill; (3) Azimuths and dips presented are those 'planned' and may vary
off collar/downhole; (4) Total Depth and collar coordinate data is preliminary.