Avrupa Minerals Intersects Polymetallic VMS Mineralization at Sesmarias

Avrupa Minerals Intersects Polymetallic VMS Mineralization at Sesmarias

(TheNewswire)

Avrupa Minerals Ltd.

  • SES24-054 cuts 41.2 meters of sulfide mineralization containing: 1.59% copper, 1.71% lead, 3.36% zinc, and 54.90 g/t silver.

- Includes 28.6 meters containing: 1.68% copper, 2.42% lead, 4.75% zinc, and 73.90 g/t silver.

  • SES24-053 cuts 13.15 meters of sulfide mineralization containing: 0.31% copper, 1.57% lead, 3.00% zinc, and 38.40 g/t silver.

- Includes 9.15 meters containing: 0.40% copper, 2.09% lead, 4.02% zinc, and 50.5 g/t silver.

  • Three of seven holes completed, with results from the first two included; results pending for third hole; fourth hole in progress.

  • Potential for two additional contingency holes; second drill on its way to the project.

Vancouver, BC, September 19, 2024 – TheNewswire - Avrupa Minerals Ltd. (TSXV: AVU) is pleased to announce the first set of analytical results from the present phase of drilling at the Sesmarias VMS Project in the Alvalade Joint Venture, Iberian Pyrite Belt, Portugal. The drilling program at Sesmarias is part of a joint venture between Avrupa Minerals and Sandfire Mineira Portugal, Unipessoal Lda. ("Sandfire Portugal"), a 100%-owned subsidiary of Minas de Aguas Teñidas, S.A. ("Sandfire MATSA") . Avrupa continues to operate the project through the JV entity PorMining Lda., and Sandfire Portugal continues to fund the exploration work.

At this time, The Company has completed three drill holes in the current Sesmarias Central program, totaling 1,715.4 meters, with a fourth hole in progress. We have seven holes planned, with the contingency of two additional holes to be drilled as/where needed. We expect a second drill in the near future to speed up the completion of this phase of drilling. To date, we have received analytical results from sampling of the first two holes (SES24-53 and SES24-054). Samples from the third hole (SES24-055) are now in the laboratory, and results are pending for these samples.

Paul W. Kuhn, President and CEO of Avrupa Minerals, stated, "These are exciting new assay results, as we continue to develop a potential high-grade polymetallic core zone in the SES Central area. The ongoing drilling program is designed to test for further high-grade copper and zinc-lead-silver mineralization along a 600-meter strike length in the Sesmarias Central zone. Extending both north and south of SES Central, known massive sulfide mineralization totals over 1,700 meters, and is open in both directions along the strike of the targeted, mineral-host black shales in the Sesmarias synform."

Results for SES24-054:

SES24-054 intercepts

From (m)

To (m)

Total (m)

Cu (%)

Pb (%)

Zn (%)

Ag (g/t)

Geological Intercept

(includes Fault breccia, massive, semi-massive replacement, stockwork sulfides)

377.2

418.4

41.2

1.59

1.71

3.36

54.90

including best copper intervals

incl.

377.2

412.4

35.2

1.78

incl.

386.8

396.8

10.0

2.24

Best Polymetallic Interval (total)

377.2

405.8

28.6

1.68

2.42

4.75

73.90

incl.

385.8

393.8

8.0

1.90

4.98

9.78

131.30

Table 1. Results for SES24-054 demonstrate further potential for high grade copper and polymetallic mineralization in the hinge zone of the Sesmarias synform in the Central area. This intersect is located approximately 150 meters SE of SES23-047, drilled last year, which intersected 26.95 meters of 2.18% Cu, 2.58% Pb, 5.60% Zn, and 88.20 g/t Ag within a wider interval of 43.40 meters of 1.51% Cu, 2.15% Pb, 4.78% Zn, and 64.1 g/t Ag. ( SES23-047 results )


Click Image To View Full Size

Figure 1. Geological cross section 800 S, looking NW, showing mineralization in SES23-048 (western limb/hinge zone) and SES24-054 (hinge zone). See Figure 3 for location of this section.

Results for SES24-053:

SES24-053 intercepts

From (m)

To (m)

Total (m)

Cu (%)

Pb (%)

Zn (%)

Ag (g/t)

Geological Intercept

Includes stockwork to semi-massive replacement sulfide mineralization

439.70

452.85

13.15

0.31

1.57

3.00

38.4

incl.

439.70

448.85

9.15

0.40

2.09

4.02

50.5

Table 2. Results for SES24-053 demonstrate polymetallic potential on the western limb of the Sesmarias synform, but perhaps distal from the hinge zone area. Similar zinc-rich, polymetallic mineralization is present in SES23-052, drilled last year, which cut the western limb some 470 meters SE of SES24-053. ( Sesmarias Results -- 2023 )


Click Image To View Full Size

Figure 2. Geological cross section 650 S, looking NW, showing mineralization in SES23-047 and SES24-053. See Figure 3 for location of this section.

Kuhn commented further, "Following the great copper and polymetallic results in SES24-054, and the strong zinc-lead-silver results in SES24-053, we are beginning to see a metal zonation centered in the SES Central hinge zone with high copper and associated base metals, transitioning outwards/upwards and along the limbs of the Sesmarias synform to more zinc-rich mineralization. Previous results in the SES North area show lower copper and stronger zinc-lead in the eastern limb of the synform, but we have yet to cross the hinge zone in the north, nor much of the western limb. The present drilling program may shed more light on the perceived metal zonation within the body of mineralization, and we look forward to more strong results."


Click Image To View Full Size

Figure 3. Contour map showing 2024 new and planned drill hole collar locations in red color and inferred massive sulfide mineralization, using drillhole interval grade (CuEq) as an exploration targeting tool . The aim of the current phase of drilling is to expand the orange-red zone in the SES Central area, and improve continuity of the high-grade, copper and polymetallic mineralization over a strike length of 600 meters, and forming a central core to the deposit.


Notes concerning Figure 3.
We use CuEq strictly as a proxy for total metal content, and as such, simply as an exploration targeting tool. In no way, are we commenting on a possible resource size or value. When reporting drill results, we utilize only individual metals' values, as reported by an accredited laboratory.

We have designed the present drill program to upgrade the +2% CuEq zone in the SES Central sector and expand the potential +2% CuEq domain into the SES North sector where historic drilling is less concentrated. Yellow and green zones generally indicate areas where historic drilling missed the target and/or recent, better-targeted drilling is sparse.

For exploration purposes, using the results from Sesmarias drilling, 2014 to present, we calculate the total amount of copper, lead, zinc, silver, and gold, without respect or indication of any/all further downstream activities, followed by calculating the value of said total metal content (in this case, as of September 10, 2024, using: Cu = US$ 4.04/lb.; Pb = US$ 0.89/lb.; Zn = US$ 1.23/lb.; Ag = US$ 28.31/oz.; and Au = US$ 2513/oz.). Finally, we calculate the equivalent content of copper, or CuEq, by dividing the value of the total contained metals by the price of copper at that time. The shape and contouring of the inferred Sesmarias mineralization, using Leapfrog geological modeling software, is courtesy of the Sandfire Portugal geological team. While metals' prices have fluctuated in a fairly narrow range since the original CuEq calculations, the shape of the VMS target area remains much the same, as it depends on metal content, not the price.

Notes on analytical methods and quality contol. T he JV analyzed the mineralized material at ALS Global facilities in Europe. For certified, NI43-101 – acceptable assay results, we selected the ME-MS61 method performed by ALS Global at their Seville sample preparation facility and Loughrea, Ireland analytical laboratory.

Due to good drilling conditions at both holes, the drillers were able to extract HQ-size (63.5 mm) core for the entire mineral intercept to get a large example of the mineralization. Project personnel collected the oriented drill core twice daily from the drill rig and delivered the boxes directly to the Project core storage facilities in Grândola, Portugal. Here, after geological and geotechnical review of the core, a Project geologist measured and marked the core for sampling, with sample length averaging one meter depending on visual factors such as change in texture, style of mineralization, and/or host rock type. Project employees systematically and methodically halved the core, utilizing an electric core saw, and then placed one half of the split material for each sample length into separate, numbered, plastic sample bags. In order to get fast, first-hand results, Project personnel transported the core samples directly to the ALS Global preparation lab in Seville, Spain.

ALS prepared the samples, using their method PREP-31by, to crush to -2mm, split off a 1-kg sample, and to pulverize to 85% passing 75 microns. The pulverized material is shipped to their main European analytical laboratory located in Loughrea, Ireland. At the analytical laboratory, we requested the samples to be analyzed via the lab's ME-MS61 technique which uses a four-acid, near-total metals' extraction method, followed by analysis using the industry-standard technique of inductively coupled plasma – atomic emission spectroscopy (ICP-AES). Another split of the pulverized material is sent to the ALS lab in Vancouver for Sn-XRF05 pressed pellet, XRF analysis to obtain a full value for tin in the drill core.

At all times, prior to submission of the samples to ALS Global, Project or Sandfire MATSA personnel maintained supervision, oversight, and custody of the samples.

In addition to ALS Global in-house quality assurance/quality control (QA/QC) for all work orders, the Project conducted its own normal, internal QA/QC from results generated by the systematic inclusion of certified reference materials, blank samples and field duplicate samples. Project personnel reviewed and evaluated the analytical results from the quality control samples in all work orders, and confirmed that these results conform to industry best practice standards.

Sandfire Portugal is a 100%-owned subsidiary of Sandfire MATSA, a modern mining company which owns and operates the MATSA Mining Operations in the Huelva province of Spain. With a processing plant located to the north of the Iberian Pyrite Belt that sources ore from three underground mines, the Aguas Teñidas and Magdalena Mines in Almonaster la Real and the Sotiel Mine in Calañas, Sandfire MATSA produces copper, zinc and lead mineral concentrates that are sold from the port of Huelva.

Avrupa Minerals Ltd. is a growth-oriented junior exploration and development company directed to discovery of mineral deposits, using a hybrid prospect generator business model. The Company holds one 49%-owned license in Portugal, the Alvalade VMS Project, presently optioned to Sandfire Portugal in an earn-in joint venture agreement. The Company holds one 100%-owned exploration license covering the Slivova Gold Project in Kosovo, optioned to Western Tethyan Resources, and is actively advancing four prospects in central Finland through its partnership with Akkerman Finland Oy. Avrupa focuses its project generation work in politically stable and prospective regions of Europe, presently including Portugal, Finland, and Kosovo. The Company continues to seek and develop other opportunities around Europe.

For additional information, contact Avrupa Minerals Ltd. at 1-604-687-3520 or visit our website at www.avrupaminerals.com .

On behalf of the Board,

"Paul W. Kuhn"

Paul W. Kuhn, President & Director

This news release was prepared by Company management, who take full responsibility for its content. Paul W. Kuhn, President and CEO of Avrupa Minerals, a Licensed Professional Geologist and a Registered Member of the Society of Mining Engineers, is a Qualified Person as defined by National Instrument 43-101 of the Canadian Securities Administrators. He has reviewed the technical disclosure in this release. Mr. Kuhn, the QP, has not only reviewed, but prepared and supervised the preparation or approval of the scientific and technical content in the news release.

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.

Copyright (c) 2024 TheNewswire - All rights reserved.

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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



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Altair Minerals Limited

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