Irka NE Assays Confirm High Grade Copper over 1.1km Strike

Irka NE Assays Confirm High Grade Copper over 1.1km Strike

Altair Minerals (ALR:AU) has announced Irka NE Assays Confirm High Grade Copper over 1.1km Strike

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High-quality and growing exploration portfolio with potential for large copper and gold deposits

Venatica Assays Confirm High-Grade Copper over 700m Strike

Venatica Assays Confirm High-Grade Copper over 700m Strike

Altair Minerals (ALR:AU) has announced Venatica Assays Confirm High-Grade Copper over 700m Strike

Download the PDF here.

Fourth Major Copper Porphyry Venatica System Discovered

Fourth Major Copper Porphyry Venatica System Discovered

Altair Minerals (ALR:AU) has announced Fourth Major Copper Porphyry Venatica System Discovered

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Altair Minerals Limited  New Central Porphyry System Identified at Venatica

Altair Minerals Limited New Central Porphyry System Identified at Venatica

Sydney, Australia (ABN Newswire) - Altair Minerals Limited (ASX:ALR) (OTCMKTS:CHKMF) is pleased to announce preliminary findings following a site visit where the Company has identified a significant outcrop of stockwork system at Central Porphyry. Outcropping quartzite, magnetite and secondary biotite veined porphyry stockwork which is part of a new separate Central Porphyry - 3km Southwest of the high-grade Irka NE Porphyry.

Key Highlights:

- Identification of new Central Porphyry | Venatica West a Porphyry Cluster

Site visit has discovered a significant outcrop of leached porphyry stockwork and ultra-potassic vein system which identifies a Central Porphyry intrusive part of a cluster system at Venatica West. Typical alteration and veining present within Bornite-Gold rich Copper Porphyry systems.

- Extremely dense veining and stockwork | Multi-stage Mineralisation

Stockwork of A-type quartz, magnetite and secondary biotite on Central Porphyry is the densest identified to date across Venatica West, suggesting significant hydrothermal activity, overlapping events, fracturing and multi-stage mineralisation at Central Porphyry, ideal for copper enrichment.

- Small portion of a much larger system | Central Porphyry Remains Open

Identification of Central Porphyry is an outstanding outcome, due to only a portion of the potassic stockwork zone outcropping, which could've easily been missed. Ultra-potassic alteration with dense stockwork as seen within this outcrop, generally tends to expand kilometres, with remaining footprint of alteration sitting under soil cover. Further fieldwork can identify full extent of this Central Porphyry.

- Potential for regional Porphyry system | SW - NE Regional Porphyry System

Preliminary fieldwork analysis on-going, with already a new Central Porphyry system being identified within virgin grounds at Venatica West, sitting ~3km Southwest of the high-grade Irka NE Porphyry and ~2km Northeast of the Irka SW Porphyry-Skarn system. Suggestive of a regional SW to NE trending porphyry cluster, filling the intersection of two district faults.

- Community Engagement Commenced | Early Community Approval

Early engagement has commenced with the local community, with multiple local members showing support for on-going exploration works. Altair's exploration team has also met with the President of the Community with very positive preliminary discussions. Altair has received initial community approval for exploration works with intention of putting forward long-term proposal of work programs, community incentive programs, project scheduling and local training.

Discovery of New Central Porphyry at Venatica West

The Central Porphyry is located on the Irka permit, situated ~3km southwest of the high-grade Irka NE Porphyry target and is a new intrusion system identified within Venatica West during initial site visit.

The upper zone of a new Central Porphyry has been identified through outcrop which consists of leached ultra-potassic stockwork of quartz, magnetite and secondary biotite dense veining, and surrounded by phyllic alteration halo and hosted within overprinted argillic alteration.

The ultra-potassic alteration suggests Altair is standing above the core of the Central Porphyry. The overprinting of strong argillic alteration has occurred from later stage hydrothermal fluids which has replaced the feldspars with clay material while maintaining the stockwork veining - suggesting a multistage mineralisation event which can significantly enrich the grades of copper sulphide and hypogene zone below. This leached stockwork from late-stage argillic alteration indicates the copper has been remobilized and disseminated into structurally favourable zones below, with potential to enhance grades within the contacts and breccia's at the core of the Central Porphyry.

The ultra-potassic zone generally sits right above the core of a Porphyry intrusion and in the case of the Central Porphyry, it is the densest set of stockwork, and veinlets discovered so far at Venatica West, with high alteration suggesting this area is the key part of hydrothermal activity and potentially the feeder to multiple other Porphyry systems.

The presence of dense secondary biotite veining on altered ultra-potassic outcrop not only indicates the presence of a new Porphyry system sitting below but also is an essential element for developing a large-scale Porphyry deposit within this particular belt.

Within other billion-tonne deposits proximal to Venatica, the presence of secondary biotite into the plays a key role in developing "scale" as its presence within porphyry stock and outwards into diorite host rock, tends to allow substitution of Fe2+ and Mg2+ with Cu2+, which can extend the copper mineral deposit footprint by a further ~500m radius in each direction from the main Porphyry core.

Key Takeaways

- Identification of new Central Porphyry akin to Bornite-Gold rich Copper Porphyries

- Ultra-potassic stockwork suggests we are standing above the core of the system

- Argillic overprint indicates a later-stage hydrothermal fluid enacted on Central Porphyry, leading to multi-phase mineralisation events.

- Leached outcrop, indicates copper has re-mobilized below into more structurally favourable zones allowing secondary enrichment in the porphyry core - which leads to higher grades.

- Presence of secondary biotite halo zone and veining in porphyry stock & diorite host is critical in developing scale within this belt for a large Cu-Au mineralisation zone beyond just the porphyry core.

- Structural alignment in SW-NE direction hosting a regional copper porphyry cluster. Irka NE Porphyry, the Central Porphyry and the SE Porphyry makes a potential corridor over more than 10km length.

This new Porphyry discovery adds on to the targets at Venatica, with 4x highly prospective undrilled targets for discovery being uncovered in this new district which is an extension of the belt which hosts multiple billion-tonne copper deposits, these targets at Venatica currently include:

- Irka NE Porphyry: Over 3.4km strike, with high-grade samples including:

- 7.0% Copper and 33g/t Silver
- 5.7% Copper and 43g/t Silver

- Irka SE Porphyry-Skarn: Large 6km2 anomalous area, with high-grade samples including:

- 4.8% Copper & 0.40g/t Gold
- 6.5% Copper & 0.52g/t Gold

- Central Porphyry: Newly discovered initial outcrop from field visit, part of a significantly larger system sitting under colluvial and soil cover. Ultra-potassic and advanced argillic alteration with significant stockwork and veining part of a separate porphyry intrusive.

- Venatica East: Over 17km of anomalous strike of copper stream sediments which are 5x background levels. Virgin grounds with potential to identify source of copper mineralisation feeding the streams and new major targets.

The identification of this Central Porphyry is significant and a result of the diligent fieldwork of the exploration team, as the outcrop is exposed over a minimal area and could've easily been missed. The degree of stockwork veining and hydrothermal activity suggests this alteration likely expands kilometres in each direction - with most of it sitting under post-mineral soil cover. Further detailed mapping and fieldwork will look to identify the true extent of this potassic alteration zone.

Venatica West is shaping up to be a regional porphyry system, hosting numerous high-quality targets for discovery. The Central Porphyry sits ~3km southwest of Irka NE and ~2km northeast of Irka SW, which indicates a structurally controlled regional porphyry trend SW - NE at Venatica West.

Community Engagement

Altair has received positive initial feedback from the community regarding its preliminary exploration activities and future plans. The community board has provided their approval and remains supportive with great relations built with local miners in the region who are eager for Altair to continue further exploration work.

Altair has also had an introduction and a very positive initial meeting with the President of the local community. Following from this, Altair representatives attended the initial community meeting and received approval to continue exploration works, with local members ready to assist. Altair continues to build upon existing supportive relationships within the community and will seek to provide a longterm formal proposal of its anticipated work programs, community incentive programs, project scheduling and local training. This proposal will be reviewed by the local community and President and will then be used to form the basis of monthly meetings with the community to build upon existing support.

Altair believes its early approach to engage the community and developing upon relationships which have been built over 10-years by the vendor of Irka will be key in fast-tracking exploration and development programs. Furthermore, this engagement is key to Altair's ESG core values and is expected to pay dividends in the future for both the Company and community. The early engagement with the community will also be critical in ensuring a smooth transition into its discovery programs.

Steps Forward at Venatica

The key anticipated steps forward aim to establish maximum value for shareholders through a scientific, systematic and diligent approach to exploration with the target of making a large-scale and globally significant discovery.

Venatica sits in the right the geological formation with all the key indicators capable of making such discovery. Altair plans to immediately initiate a comprehensive program to further evaluate the full potential of Venatica. The next key steps as part of the Venatica execution program includes:

- Evaluation of regional potential and detailed mapping

- On-going community engagement at Venatica West & Venatica East

- Rock chip and geochemical sampling program at Venatica West

Altair Chief Executive Officer, Faheem Ahmed comments:

"This is an outstanding find by our geological team within the high-grade Venatica Copper Project. This is now our third Porphyry target at Venatica West, and we are treading virgin and unexplored grounds here with potential to discover further mineralised outcrops and Porphyry's.

There is consistent dense veining across the outcrop which is exactly what you would like to see within a porphyry intrusion, suggesting significant magmatic fluid activity. More importantly, it appears the Central Porphyry has gone through multi-stage mineralisation, which not only introduces more copper into the intrusion, but also indicates copper has been leached from the outcrop and has potential to go through secondary enrichment below. These are all key indicators we are onto an exceptional exploration target, both with scale and potential to be high-grade.

We now have three key targets at Venatica West, two of them which has shown exceptional copper grades ranging 4 - 9% at surface across a large area. With the latest addition being this Central Porphyry, which has gone through significant leaching. Due to the leaching, we're looking for anomalous levels of copper at surface within the Central Porphyry, which will confirm to us this stockwork is likely to be significant mineralised at depth from remobilization of copper ions.

Furthermore, we are yet to even touch Venatica East, which hosts 17km strike of anomalous copper stream sediments. I'm incredibly excited to get boots on ground at Venatica East which is a pure greenfield opportunity and has never been systematically treaded or even sampled, and no one has ever followed up these prominent copper anomalies. We'll be the first Company to take an experienced geological team down to Venatica East, so the possibilities and upside is quite endless.

Simultaneously, we continue to progress works at Olympic Domain, our latest announcement on the project, 4 December 2024, has indicated a robust conductive ovoid, with historic drilling narrowly missing the core of the target. We are in intending to complete a follow-up TEM survey which can identify the precise depth of this ovoid, which will be critical for our drill program and targeting."

*To view tables and figures, please visit:
https://abnnewswire.net/lnk/BB53832O



About Altair Minerals Limited:  

Altair Minerals Limited (ASX:ALR) (OTCMKTS:CHKMF) is listed on the Australian Securities Exchange (ASX) with the primary focus of investing in the resource sector through direct tenement acquisition, joint ventures, farm in arrangements and new project generation. The Company has projects located in South Australia, Western Australia and Queensland with a key focus on its Olympic Domain tenements located in South Australia.



Source:
Altair Minerals Limited

News Provided by ABN Newswire via QuoteMedia

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Group Eleven Intersects 7.5m of 20.1% Zn+Pb and 51 g/t Ag, incl. 2.2m of 37.5% Zn+Pb and 72 g/t Ag at Ballywire in Step-Out Drilling; Upcoming Drilling at Cu-Ag Target and 'D' Gravity Anomaly

Group Eleven Intersects 7.5m of 20.1% Zn+Pb and 51 g/t Ag, incl. 2.2m of 37.5% Zn+Pb and 72 g/t Ag at Ballywire in Step-Out Drilling; Upcoming Drilling at Cu-Ag Target and 'D' Gravity Anomaly

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) ("Group Eleven" or the "Company") is pleased to announce assay results from four new holes (and additional assays from a previously announced hole) from the ongoing drill program at the Company's 100%-owned Ballywire zinc-lead-silver discovery ("Ballywire"), PG West Project ("PG West"), Republic of Ireland.

Highlights:

  • G11-3552-29 intersected (from 189.3m):
    • 130.7m of 2.3% Zn+Pb (2.0% Zn and 0.3% Pb) and 13 g/t Ag, including
    • 7.5m of 20.1% Zn+Pb (19.1% Zn and 1.0% Pb) and 51 g/t Ag, including
    • 5.7m of 24.1% Zn+Pb (23.2% Zn and 1.0% Pb) and 60 g/t Ag, including
    • 2.2m of 37.5% Zn+Pb (36.9% Zn and 0.7% Pb) and 72 g/t Ag
    • 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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https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_002full.jpg

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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https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_003full.jpg

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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Questcorp Mining Plans IP Survey at North Island Copper

Questcorp Mining Plans IP Survey at North Island Copper

Questcorp Mining Inc. (CSE: QQQ) (OTCQB: QQCMF) (FSE: D910) (the "Company" or "Questcorp") is pleased to announce permitting is under way for a 10 to 15 line km induced polarization (IP) survey at the Company's 1,168 hectare North Island Copper project near Port Hardy on Vancouver Island, British Columbia.

While Questcorp's North Island Copper project hosts 8 targets across the property, the main target is the historic Marisa Zone, a porphyry copper target last explored in the 1990's. Surface sampling and a preliminary 12.3-line km Induced Polarization (IP) survey identified an interesting chargeability anomaly that was followed up by a five hole, 376.43 diamond drilling program. Two of the five holes hit interesting copper values including down hole intervals of 0.078% copper over 56.39 metres in DDH92-01 and 0.041% copper over 70.71 metres in DDH92-03 in an altered quartz diorite. Copper grades were increasing with depth in DDH92-03. The Company plans to follow up these historic results.

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Heritage Provides Exploration Update on New Millennium Prospect

Heritage Provides Exploration Update on New Millennium Prospect

(TheNewswire)

Heritage Mining Ltd.

NOT INTENDED FOR DISTRIBUTION TO UNITED STATES NEWS WIRE SERVICES OR FOR DISSEMINATION IN THE UNITED STATES

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The White House introduces Immediate and Vigorous Measures to fast track the Domestic Mining Industry and Production

The White House introduces Immediate and Vigorous Measures to fast track the Domestic Mining Industry and Production

(TheNewswire)

Noble Mineral Exploration Inc.

TORONTOTheNewswire - March 2 4 2025 - Noble Mineral Exploration Inc. (" Noble " or the " Company ") (TSXV: NOB) (OTCQB: NLPXF) is pleased to report that t he White House announced immediate measures to be introduced to significantly increase the US production of lithium, nickel, copper, and rare earths, with an eye to increased production, the creation of jobs and, significantly, the reduction of US reliance on foreign nations.

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Silver47 Announces Closing of Third Tranche and Upsize of Non-Brokered Private Placement from $8 Million to $11 Million

Silver47 Announces Closing of Third Tranche and Upsize of Non-Brokered Private Placement from $8 Million to $11 Million

Silver47 Exploration Corp. (TSXV: AGA) (OTCQB: AAGAF) ("Silver47" or the "Company") is pleased to announce that, due to strong investor demand, it has increased the size of its previously announced non-brokered private placement (the "Private Placement") from $8 million to $11 million (the "Upsize"). The Company also intends to complete the third tranche (the "Third Tranche") of the Private Placement on March 21, 2025. The closing of the Third Tranche, along with the Upsize, will be completed as part of the same financing, as set out in the Company's news releases dated February 19 and 24, 2025.

Pursuant to the Third Tranche, the Company will issue approximately 3,871,000 units at a price of $0.50 each, for gross proceeds of approximately $1,935,500. Completion of the Third Tranche will result in the Company having issued an aggregate of 14,938,400 units and 929,192 flow-through units (at a price of $0.57 per flow-through unit) for aggregate proceeds under the Private Placement of $7,998,839.

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