PAN GLOBAL ONGOING DRILLING EXTENDS STRIKE OF LA ROMANA NEAR-SURFACE COPPER-TIN-SILVER MINERALIZATION TO 1.35 KILOMETERS

PAN GLOBAL ONGOING DRILLING EXTENDS STRIKE OF LA ROMANA NEAR-SURFACE COPPER-TIN-SILVER MINERALIZATION TO 1.35 KILOMETERS

TSXV: PGZ | OTCQX: PGZFF

  • Romana West drilling extends La Romana mineralization 150m to the west
  • Copper-tin grades increasing to the west
  • Investor webcast with CEO Tim Moody to discuss results will be held on Wednesday, September 20, 2023 at 11 a.m. Eastern Time / 8 a.m. Pacific Time . Details at end of this release

Pan Global Resources Inc. ("Pan Global" or the "Company") (TSXV: PGZ) (OTCQX: PGZFF) is pleased to announce assay results for the first six holes drilled at the Romana West target, testing extensions to the La Romana copper-tin-silver discovery at the Company's 100% owned Escacena Project in the Iberian Pyrite Belt in southern Spain .

Key highlights:
  • Copper and tin mineralization with good continuity starts immediately below a thin cover of sediments
  • Moderately north-dipping tabular geometry ideally suited for potential open-pit mining
  • High value tin grades increasing to the west
  • LRD162 intercepted 17m at 0.65% CuEq 1 ( 0.4% Cu 0.13% Sn, 1.1 g/t Ag) from 50.0m , including 6m at 1.24% CuEq 1 (0.5% Cu, 0.29% Sn, 1.5g/t Ag)
  • LRD166 intercepted 14.5m at 0.75 % CuEq 1 (0.36% Cu, 0.15% Sn, 1.2 g/t Ag from 7.5m , including 5m at 1.06% CuEq 1 (0.48% Cu, 0.21% Sn, 2.0 g/t Ag)
  • LRD164 intercepted 16m at   0.70% CuEq 1 (0.52 % Cu, 0.06 % Sn, 1.6 g/t Ag) from 37.0m , including   3m   at 1.38% CuEq 1 (1.06% Cu, 0.11% Sn, 3.9 g/t Ag)
  • Mineralization remains wide open at depth and to the west
  • Drilling ongoing with results pending from six additional completed drill holes with visual copper and tin mineralization

Drill hole locations are shown in Figure 1 below. Drill hole assay results are summarized in Table 1 and collar details are presented in Table 2 below.

"Drilling at Romana West commenced within weeks of being granted surface access. Twelve of our planned 25 drill holes have been completed and assay results for the first six are very encouraging. Our drill program has been highly successful, confirming continuity of the copper-tin-silver mineralization 150 meters to the west of the La Romana discovery. The overall strike length of La Romana is now 1.35 kilometers and is still open, with step-out drilling continuing farther to the west. Results to date show the potential for grades to increase to the west," said Tim Moody , President and CEO of Pan Global.

The Romana West mineralization occurs in two main layers, Zone B and Zone C, commencing directly below a thin cover of post mineral sediments. Sulphide mineralization was intersected in all holes at depths predicted from modelling of previous drilling and geology data. At shallow depths the primary sulphides, including chalcopyrite and pyrite, have been overprinted by supergene chalcocite and copper enrichment.

The assay results also include some of the highest tin grades reported in the Escacena project area, with assays up to 0.62% Sn. Coarse cassiterite was observed in both Zone B and Zone C. Importantly, cassiterite is the only tin mineral observed and is preferred for metallurgical extraction to produce a valuable tin concentrate. Processed tin is a key ingredient in electronics and solar panels and regularly trades at three-to-four times the value of processed copper.

The ongoing drill program aims to test the near-surface La Romana mineralization a further 350m along strike to the west.

Figure 1 – Gravity anomaly map showing the Romana West and La Romana targets, drill hole locations with selected results, and cross-section locations A-A' (Figure 2) and B-B' (Figure 3).

Figure 1 – Gravity anomaly map showing the Romana West and La Romana targets, drill hole locations with selected results, and cross-section locations A-A' (Figure 2) and B-B' (Figure 3). (CNW Group/Pan Global Resources Inc.)

Figure 2 – Cross section 736010m East, A-A', showing selected assay results highlights and copper grade shells for new drill holes LRD161 , LRD162 and LRD166 , with mineralization commencing immediately beneath the post mineral cover to nearly 200m down-dip (to the north).

Figure 2 – Cross section 736010m East, A-A', showing selected assay results highlights and copper grade shells for new drill holes LRD161, LRD162 and LRD166, with mineralization commencing immediately beneath the post mineral cover to nearly 200m down-dip (to the north). (CNW Group/Pan Global Resources Inc.)

Figure 3 – Cross section 735900m East, B-B', showing selected highlights and copper grade shells for new drill holes LRD163 , LRD164 and LRD165 .

Figure 3 – Cross section 735900m East, B-B', showing selected highlights and copper grade shells for new drill holes LRD163, LRD164 and LRD165. (CNW Group/Pan Global Resources Inc.)

Table 1 – Romana West drill results summary

Hole ID

From

To

Interval

CuEq( 1 )

Cu

Sn

Ag


Au

Pb

Zn

True
Thickness


m

m

m

%

%

%

g/t


g/t

ppm

ppm

(m)

LRD161

117.00

130.00

13.00

0.27

0.25

0.01

0.8


0.01

11

72

11.79

Including

126.00

130.00

4.00

0.49

0.46

0.01

1.6


0.01

19

85

3.63

and

150.00

162.00

12.00

0.36

0.28

0.03

1.1


0.01

7

70

10.9

Including

150.00

156.00

6.00

0.60

0.47

0.05

1.9


0.01

12

79

5.44

Including

152.00

153.00

1.00

1.61

1.23

0.14

4.0


0.01

21

87

0.91

LRD162

50.00

67.00

17.00

0.65

0.30

0.13

1.1


0.01

49

81

17.00

Including

52.00

58.00

6.00

1.24

0.47

0.29

1.5


0.01

19

75

6.00

and

95.00

109.15

14.15

0.27

0.18

0.03

0.6


0.02

10

64

14.15

Including

107.00

109.15

2.15

0.63

0.46

0.06

2.1


0.088

36

76

2.15

and

132.50

135.00

2.50

0.89

0.10

0.30


0.01

42

58

2.50

Including

134.00

135.00

1.00

1.64

0.62


0.01

6

47

1.00

LRD163

30.35

32.00

1.65

0.86

0.76

0.03

3.7


137

103

1.27

and

60.00

72.00

12.00

0.31

0.25

0.02

2.2


0.01

80

142

9.20

and

122.00

126.00

4.00

0.29

0.23

0.02

0.5


3

50

3.07

LRD164

37.00

53.00

16.00

0.70

0.52

0.06

1.6


0.01

7

85

16.00

Including

43.00

47.00

4.00

0.93

0.68

0.09

1.8


0.01

2

91

4.00

Including

49.00

52.00

3.00

1.38

1.06

0.11

3.9


0.02

16

78

3.00

and

87.00

91.00

4.00

0.66

0.52

0.05

0.8


0.02

3

51

4.00

Including

88.00

89.00

1.00

1.59

1.42

0.06

2.0


0.05

8

50

1.00

LRD165

86.25

87.70

1.45

0.64

0.36

0.10

1.2


0.01

5

87

1.24

and

114.00

122.85

8.85

0.59

0.55

0.01

1.4


0.008

6

74

7.58

Including

119.00

122.85

3.85

1.08

1.04

0.013

2.7


0.013

10

80

3.3

Including

122.25

122.85

0.60

5.24

5.06

0.04

13.0


0.034

29

180

0.51

LRD166

7.50

22.00

14.50

0.75

0.36

0.15

1.2


0.012

25

129

13.30

including

17.00

22.00

5.00

1.06

0.48

0.21

1.5


0.018

27

131

4.6

and

72.00

73.20

1.20

1.19

1.04

0.06

1.7


0.024

11

48

1.10

1   Copper Equivalent = CuEq. CuEq is calculated using Cu, Sn, and Ag grades. Metallurgical recoveries of 86% for Cu, 68% for Sn and 56% for Ag are based on preliminary studies performed by Wardell Armstrong International and MinePro. The CuEq calculation assumes commodity prices of US$ 8,693/tonne Cu, US$ 29,069/tonne Sn and US$ 23.72/oz Ag, corresponding to the three-year monthly price averages to July 2023. The effective formula is [CuEq %] = [Cu %] + 2.6440 * [Sn %] + 0.0057 * [Ag ppm]

Table 2 – Romana West drill hole collar information (6 holes, total 1,004.95m )

Hole ID

Easting 2

Northing 2

Azimuth ( o )

Dip( o )

Depth (m)

LRD161

736025.3

4152813

195

-70

197.45

LRD162

735989.1

4152760

180

-50

182.05

LRD163

735921.6

4152767

180

-90

167.9

LRD164

735921.7

4152766

180

-50

140.35

LRD165

735895.7

4152851

156

-70

222.45

LRD166

736038.8

4152687

156

-55

94.75

2 Coordinate system. UTM29N ERTS89

Investor Call to Discuss Drill Results and Expanding La Romana

CEO Tim Moody will host a conference call and webcast on Wednesday, September 20, 2023 , at 11:00 a.m. Eastern Time / 8:00 a.m. Pacific Time to discuss the latest results at the Escacena Project. An open Q&A session will follow a short presentation.

Date: Wednesday, September 20, 2023
Time: 11:00 a.m. Eastern Time | 8:00 a.m. Pacific Time
Please register in advance: https://us06web.zoom.us/meeting/register/tZEtcumhrzsqE9XnLSo4hLpyYL7Nrdq-utim .

After registering, you will receive a confirmation email containing information about joining the meeting. Investors are encouraged to send questions or topics of interest in advance to investors@panglobalresources.com to be addressed following the presentation. A link to the webcast will be available on the Company's website at https://panglobalresources.com following the live broadcast.

About the Escacena Project

The Escacena Project comprises a large, contiguous, 5,760-hectare land package controlled 100% by Pan Global in the east of the Iberian Pyrite Belt. Escacena is located near operating mines at Las Cruces and Riotinto and is immediately adjacent to the former Aznalcóllar and Los Frailes mines where Minera Los Frailes/Grupo Mexico is in the final permitting stage with construction anticipated to start in 2023. The Escacena Project hosts the La Romana copper-tin-silver discovery and a number of other prospective targets, including Zarcita, Hornitos, La Jarosa, Romana Deep , Romana North , Romana West, Cañada Honda, Bravo, Barbacena, El Pozo, and San Pablo.

Pan Global Resources Inc. is actively targeting copper-rich mineral deposits, given copper's compelling supply-demand fundamentals and outlook for strong long-term prices as a critical metal for global electrification and energy transition. The Company's flagship Escacena Project is located in the prolific Iberian Pyrite Belt in southern Spain , where infrastructure, mining and professional expertise, and support for copper as a Strategic Raw Material by the European Commission collectively define a tier-one jurisdiction for mining investment. The Pan Global team comprises proven talent in exploration, development, and mine operations - all of which are committed to operating safely and with utmost respect for the environment and our partnered communities.

QA/QC Procedures

Core size was HQ (63mm) and all samples were ½ core. Nominal sample size was 1m core length and ranged from 0.5 to 2m . Sample intervals were defined using geological contacts with the start and end of each sample physically marked on the core. Diamond blade core cutting and sampling was supervised at all times by Company staff. Duplicate samples of ¼ core were taken approximately every 30 samples and Certified Reference materials inserted every 25 samples in each batch.

Samples were delivered to ALS laboratory in Seville, Spain and assayed at the ALS laboratory in Ireland . All samples were crushed and split (method CRU-31, SPL22Y), and pulverized using (method PUL-31). Gold analysis was by 50gm Fire assay with ICP finish (method Au-ICP22) and multi element analysis was undertaken using a 4-acid digest with ICP AES finish (method ME-ICP61). Over grade base metal results were assayed using a 4-acid digest ICP AES (method OG-62). Over grade tin was determined using peroxide fusion with ICP finish (method Sn-ICP81x).

Qualified Persons

James Royall , Vice President Exploration for Pan Global Resources and a qualified person as defined by National Instrument 43-101, has reviewed the scientific and technical information for this news release. Mr. Royall is not independent of the Company.

On behalf of the Board of Directors

www.panglobalresources.com

Forward-looking statements

Statements which are not purely historical are forward-looking statements, including any statements regarding beliefs, plans, expectations or intentions regarding the future. It is important to note that actual outcomes and the Company's actual results could differ materially from those in such forward-looking statements. The Company believes that the expectations reflected in the forward-looking information included in this news release are reasonable but no assurance can be given that these expectations will prove to be correct and such forward-looking information should not be unduly relied upon. Risks and uncertainties include, but are not limited to, economic, competitive, governmental, environmental and technological factors that may affect the Company's operations, markets, products and prices. Readers should refer to the risk disclosures outlined in the Company's Management Discussion and Analysis of its audited financial statements filed with the British Columbia Securities Commission.

The forward-looking information contained in this news release is based on information available to the Company as of the date of this news release. Except as required under applicable securities legislation, the Company does not intend, and does not assume any obligation, to update this forward-looking information.

NEITHER TSX VENTURE EXCHANGE NOR ITS REGULATION SERVICES PROVIDER (AS THAT TERM IS DEFINED IN THE POLICIES OF THE TSX VENTURE EXCHANGE) ACCEPTS RESPONSIBILITY FOR THE ADEQUACY OR ACCURACY OF THIS RELEASE.

Pan Global Resources Inc. logo (CNW Group/Pan Global Resources Inc.)

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SOURCE Pan Global Resources Inc.

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  • G11-3552-29 intersected (from 189.3m):
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    • Represents a 55m step-out down-dip from G11-3552-27
  • G11-3552-271 intersected (from 201.5m):
    • 70.5m of 3.4% Zn+Pb (2.2% Zn and 1.2% Pb) and 41 g/t Ag, including
    • 25.7m of 7.9% Zn+Pb (5.7% Zn and 2.2% Pb), 78 g/t Ag and 0.12% Cu and
    • 4.2m of 2.0% Zn+Pb (0.4% Zn and 1.6% Pb), 172 g/t Ag and 0.66% Cu, including
    • 0.9m of 3.6% Zn+Pb (0.9% Zn and 2.6% Pb), 511 g/t Ag and 2.01% Cu
    • Located 50m down-dip from G11-3552-25 (announced 06-Feb-2025)
  • G11-3552-29 expands the footprint of the recently announced 360m long, flat-lying zone of zinc-rich massive sulphide lenses by at least 50m down-dip, to a total of at least 125m down-dip
  • Drilling continues at Ballywire with two rigs testing further down-dip of the two holes released today, plus the NE extension; assay results are expected in due course
  • In several weeks, drilling will also begin testing (a) a Cu-Ag target below the Zn-Pb-Ag discovery horizon; and (b) a step-out target 1.3km to the ENE of the Ballywire discovery testing in the vicinity of the prospective 'D' gravity-high anomaly, at a locality with abundant calcite similar to the calcite typically observed immediately above high-grade mineralization along the discovery trend

"We are very pleased to see the NE massive sulphide zone expanded by a ninth consecutive high-grade hole," stated Bart Jaworski, CEO. "Additional excellent Ag and Cu values also continue to point to a stratigraphically deeper Cu-Ag horizon, which we are aiming to start drill testing for the very first time over the next few weeks. We also look forward to stepping out 1.3km ENE towards a very prospective area near the 'D' gravity high anomaly. This locality hosts abundant calcite bodies, commonly seen above high-grade mineralization at Ballywire. A nearby historic hole is also mineralized. With the Cu-Ag target, continued drilling to the NE and larger step outs along our prospective 6km trend, 2025 promises to be an exciting year of exploration for Group Eleven."

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Exhibit 1. Cross-Section Showing New Drilling (G11-3552-27, -29 and -31) at Ballywire Discovery

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Note: Partial assays from G11-3552-27 previously announced on 06-Feb-25, consisting of 24.8m of 8.1% Zn+Pb, 80 g/t Ag;

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Exhibit 2. Plan Map Showing New Drilling and Interpreted Cu-Ag 'Feeder' Structure

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Note: Partial assays from G11-3552-27 previously announced on 06-Feb-25, consisting of 24.8m of 8.1% Zn+Pb, 80 g/t Ag;

New Step-Out Holes at Ballywire Discovery

The Ballywire prospect at the Company's 100%-owned PG West Project in Republic of Ireland, is a relatively new zinc-lead-silver discovery (first announced Sept-2022). In addition to 44 holes drilled and reported by Group Eleven to date, the most recent four holes (G11-3552-24, -26, -28, and -29) and additional assays for previously announced hole, G11-3552-27, are reported today (see Exhibits 1 to 7).

High-grade mineralization from G11-3552-27 and -29 (see Page 1 and Exhibits 1 to 4) consists predominantly of massive and semi-massive sulphide (sphalerite, galena, pyrite, chalcopyrite and suspected tennantite-tetrahedrite), as well as, disseminated and vein hosted sulphide mineralization. Mineralization occurs along and/or close to the base of the Waulsortian Limestone (see Exhibit 1).

Exhibit 3. Summary of Assays from G11-3552-24, -26, -27, -28 and -29 at Ballywire

ItemFrom
(m)
To
(m)
Int
(m)
Zn
(%)
Pb
(%)
Zn+Pb
(%)
Ag
(g/t)
Cu
(%)
G11-3552-27201.45271.9470.492.221.203.4140.80.09
Incl.212.07237.8125.745.692.217.9077.80.12
Incl.219.42235.0615.648.303.2811.59122.10.19
Incl.218.47222.213.7412.183.0515.2375.3-
And228.51235.066.5511.065.6516.71240.00.42
Incl.230.36233.903.5413.268.0121.27395.10.73
And267.72271.944.220.401.581.97171.60.66
Incl.268.64269.490.850.932.623.55511.02.01
G11-3552-29189.33320.05130.721.990.262.2513.0-
Incl.224.27229.615.344.100.794.8812.5-
And259.03266.567.5319.081.0120.0951.3-
Incl.259.03264.745.7123.160.9524.1160.0-
Incl.259.03261.252.2236.860.6837.5471.7-
And307.91320.0512.140.230.040.2766.20.12
Incl.315.26320.054.790.380.050.42149.40.27
Incl.318.00320.052.050.090.040.12301.00.52
G11-3552-24186.26199.2012.940.150.040.192.1-
Incl.193.76197.313.550.300.100.404.8-
And235.85236.760.910.010.010.0136.10.35
G11-3552-26215.80216.360.560.830.791.6271.5-
Incl.215.80215.970.172.522.254.77190.0-
G11-3552-28157.95174.8116.860.020.580.593.1-
Incl.166.42169.282.860.051.261.319.0-
And172.99174.811.820.072.122.196.8-
And179.67181.491.820.030.170.2064.10.16
And218.66220.501.840.000.000.012.70.26

 

Note: True width of the intervals above as a percentage of the intersected interval is 90% (G11-3552-27), 80-90% (G11-3552-29), 90-100% (G11-3552-24), 80-90% (G11-3552-26) and 90-100% (G11-3552-28)

Holes drilled as 300m step-outs to the NE (G11-3552-24, -26 and -28; see Exhibit 2) returned zones of mineralization narrower and weaker than those at the main discovery trend (see Exhibit 3). Disseminated copper mineralization, as well as, mineralized veins and fractures, however, are strengthening towards the north, suggesting massive sulphide mineralization may be present further north (see northern-most projected mineralized trend in Exhibit 4). A second mineralized trend is also emerging to the south where the interpreted Cu-Ag rich 'feeder' fault pierced by drilled along the main discovery trend (see solid purple line in Exhibits 2 and 4) appears to correlate with mineralization intersected in G11-3552-08 (see Exhibit 2). More drilling is ongoing in the NE area to test the above targets.

Key 2025 Exploration Targets at Ballywire Discovery

Copper-Silver Target

As drilling progresses at Ballywire, it is increasingly evident that there exists an interpreted Cu-Ag 'feeder' fault parallel to and spatially associated with the main Zn-Pb-Ag discovery at Ballywire (see Exhibit 2). This 'feeder' fault hosts mineralization with up to 5.90% Cu and 1,440 g/t Ag, interpreted to have been transported by mineralizing fluids from below by vertical to steeply-dipping structures (see Exhibit 5). Today's results provide further evidence, with grades up to 2.01% Cu and 511 g/t Ag (see Exhibit 3). Meanwhile, the stratigraphy of the region suggests that approximately 100-200m below the discovery horizon (base of the Waulsortian Limestone), is the Lower Limestone Shale horizon, which hosts four well known Cu-Ag historic occurrences in the surrounding area (see Denison, Oola, Gortdrum and Tullacondra in Exhibit 8, located approx. 5km, 9km, 10km and 45km away from Ballywire, respectively).

These historic Cu-Ag occurrences can be interpreted as the eroded remnants of originally more vertically extensive mineralizing systems, likely representing the roots of stratigraphically higher Zn-Pb-Ag mineralization. At Ballywire, there is a chance the mineralizing system is much larger than at the neighbouring deposits (based on relatively large footprint to date), and if it is there, any Cu-Ag mineralization would notionally be intact below the existing Zn-Pb-Ag mineralization.

Given the compelling nature of the above exploration model, Group Eleven aims to begin drilling this deeper Cu-Ag target over the coming several weeks.

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Exhibit 4. Plan Map Showing Interpreted Cu-Ag 'Feeder' and Calcite Body Targets at Ballywire

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Note: Calcite bodies occurring at the discovery trend are not shown here (shown in Exhibit 6 instead)

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Exhibit 5. Cross-Section Showing Hypothesized Location of Cu-Ag Mineralization

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Calcite Body Vectors

As drilling progresses at Ballywire, it is increasingly evident that high-grade Zn-Pb-Ag mineralization at Ballywire is spatially associated with steeply dipping bodies of calcite (see Exhibit 6), interpreted to represent the 'exhaust' from the mineralization process below (i.e. dissolved limestone at the mineralized horizon is re-precipitated as calcite bodies immediately above). These calcite bodies may prove to be a strong exploration vector along the undrilled remainder of Ballywire's prospective 6km trend.

Two shallow historic holes, located 1.3km ENE from the current boundary of the Ballywire discovery, intercepted such calcite bodies (see Exhibits 4 and 7), yet were never followed up. This locality is also near the prospective 'D' gravity high anomaly and historic hole, 99-3352-05 (see Exhibit 7), which intersected mineralization of a tenor typically seen peripheral to massive sulphide zones at the discovery trend. Group Eleven aim to test this locality in the coming weeks.

Separately, two historic holes approx. 300m and 600m to the WSW, respectively, from the current boundary of the Ballywire discovery, also intercepted abundant calcite zones (see Exhibits 4 and 7) and were never followed up. Group Eleven aims to test these locations in due course.

Looking forward, six (6) drill holes (G11-3552-30 to -35; see Exhibit 2) are in progress with results expected in due course. Exhibit 2 shows drilling to date across 1.25km of the overall 2.6km long trend (see Exhibit 4) of significantly mineralized drill intercepts. This in turn is hosted within a 6km long prospective trend defined by four gravity high anomalies, only one of which (anomaly 'C') is systematically drilled to date (see Exhibit 7).

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Exhibit 6. Oblique 3D View of Calcite Bodies Spatially Associated with Mineralization at Ballywire

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Note: Bodies shown (calcite, Zn-Pb-Ag and Cu-Ag) are not constrained by any grade cut-off and are only meant for illustrative purposes

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Exhibit 7. Regional Gravity at Ballywire Showing 6km Long Prospective Trend and Calcite Bodies

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Notes to Exhibit 8: (a) Pallas Green MRE is owned by Glencore (see Glencore's Resources and Reserves Report dated December 31, 2023); (b) Stonepark MRE: see the 'NI 43-101 Independent Report on the Zinc-Lead Exploration Project at Stonepark, County Limerick, Ireland', by Gordon, Kelly and van Lente, with an effective date of April 26, 2018, as found on SEDAR; and (c) the historic estimate at Denison was reported by Westland Exploration Limited in 'Report on Prospecting Licence 464' by Dermot Hughes dated May, 1988; the historic estimate at Gortdrum was reported in 'The Geology and Genesis of the Gortdrum Cu-Ag-Hg Orebody' by G.M. Steed dated 1986; and the historic estimate at Tullacondra was first reported by Munster Base Metals Ltd in 'Report on Mallow Property' by David Wilbur, dated December 1973; and later summarized in 'Cu-Ag Mineralization at Tullacondra, Mallow, Co. Cork' by Wilbur and Carter in 1986; the above three historic estimates have not been verified as current mineral resources; none of the key assumptions, parameters and methods used to prepare the historic estimates were reported and no resource categories were used; significant data compilation, re-drilling and data verification may be required by a Qualified Person before the historic estimates can be verified and upgraded to be compliant with current NI 43-101 standards; a Qualified Person has not done sufficient work to classify them as a current mineral resource and the Company is not treating the historic estimates as current mineral resources. 'Rathdowney Trend' is the south-westerly projection of the Rathdowney Trend, hosting the historic Lisheen and Galmoy mines.

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Exhibit 8. Regional Map of Ballywire Discovery and Surrounding Cu-Ag Historic Occurrences

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Qualified Person

Technical information in this news release has been approved by Professor Garth Earls, Eur Geol, P.Geo, FSEG, geological consultant at IGS (International Geoscience Services) Limited, and independent 'Qualified Person' as defined under Canadian National Instrument 43-101.

Sampling and Analytical Procedures

All core drilled at Ballywire is NQ (47.6mm) and is cut using a rock saw. Sample intervals vary between 0.42m to 1.3m with the majority of samples in the 0.79m to 0.99m range. The half-core samples are bagged, labelled and sealed at Group Elevens core store facility in Limerick, Ireland. Selected sample bags are examined by the Qualified Person. Transport is via an accredited courier service and/or by Group Eleven staff to ALS Laboratories in Loughrea Co. Galway, Ireland. Sample preparation at the ALS facility comprises fine crushing 70%

Quality Assurance/Quality Control (QA/QC) Information

Group Eleven inserts certified reference materials ("CRMs" or "Standards") as well as blank material, to its sample stream as part of its industry-standard QA/QC programme. The QC results have been reviewed by the Qualified Person, who is satisfied that all the results are within acceptable parameters. The Qualified Person has validated the sampling and chain of custody protocols used by Group Eleven.

About Group Eleven Resources

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) and (FSE: 3GE) is a mineral exploration company focused on advanced stage zinc exploration in the Republic of Ireland. Group Eleven announced the Ballywire discovery in September 2022. Key intercepts to date include:

  • 10.8m of 10.0% Zn+Pb and 109 g/t Ag (G11-468-03)
  • 10.1m of 8.6% Zn+Pb and 46 g/t Ag (G11-468-06)
  • 10.5m of 14.7% Zn+Pb, 399 g/t Ag and 0.31% Cu (G11-468-12)
  • 11.2m of 8.9% Zn+Pb and 83 g/t Ag (G11-3552-03)
  • 29.6m of 10.6% Zn+Pb, 78 g/t Ag and 0.15% Cu (G11-3552-12) and
  • 11.8m of 11.6% Zn+Pb, 48 g/t Ag (G11-3552-18)
  • 15.6m of 11.6% Zn+Pb, 122 g/t Ag and 0.19% Cu (G11-3552-27)

Ballywire is located 20km from Company's 77.64%-owned Stonepark zinc-lead deposit2, which itself is located adjacent to Glencore's Pallas Green zinc-lead deposit3. The Company's two largest shareholders are Glencore Canada Corp. (16.1% interest) and Michael Gentile (16.0%). Additional information about the Company is available at www.groupelevenresources.com.

ON BEHALF OF THE BOARD OF DIRECTORS

Bart Jaworski, P.Geo.
Chief Executive Officer

E: b.jaworski@groupelevenresources.com | T: +353-85-833-2463
E: j.webb@groupelevenresources.com | T: 604-644-9514

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Information

This press release contains forward-looking statements within the meaning of applicable securities legislation. Such statements include, without limitation, statements regarding the future results of operations, performance and achievements of the Company, including the timing, content, cost and results of proposed work programs, the discovery and delineation of mineral deposits/resources/ reserves and geological interpretations. Although the Company believes that such statements are reasonable, it can give no assurance that such expectations will prove to be correct. Forward-looking statements are typically identified by words such as: believe, expect, anticipate, intend, estimate, postulate and similar expressions, or are those, which, by their nature, refer to future events. The Company cautions investors that any forward-looking statements by the Company are not guarantees of future results or performance, and that actual results may differ materially from those in forward looking statements as a result of various factors, including, but not limited to, variations in the nature, quality and quantity of any mineral deposits that may be located. All of the Company's public disclosure filings may be accessed via www.sedarplus.com and readers are urged to review these materials, including the technical reports filed with respect to the Company's mineral properties.

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