DISCOVERY OF TWO NEW MINERALIZED ZONES AT BLUE LAKE PROJECT
Highlights of the 2025 Fieldwork (figure 1)
- 457 grab samples were collected, primarily from outcrop and felsenmeers (in-situ angular blocks formed by freezing-thawing cycles, representing the underlying outcrop)
- Discovery of two new mineralised zones: North Retty and Retty Lake Northwest
- Several sectors assayed between 0.4 and 0.83% Cu eq, the same range of values obtained from the surface sampling over the known Cu-Ni-PGE deposits.
- The observation of net textured sulphides and sulphides blebs in several areas may indicate the proximity of Cu-Ni-PGE mineralisation
- Extension of the surface expression of the
Blue Lake mineralized area to the South and the South-East. - All surface mineralized occurrences correspond to combined magnetic and electromagnetic anomalies.
New Zones
Retty Lake Northwest
At the northwest end of
North Retty
North of the Retty Lake Camp, two ultramafic felsenmeer blocks were discovered at the northern edge of an interpreted ultramafic sequence. Both blocks exhibited net textured sulphides, and one had a few small chalcopyrite-rich blebs. Assay results are 0.55% and 0.52% Cu eq. A third very rusty block, located 2 km to the south-east, along the same ultramafic unit, graded 0.45% Cu equivalent.
Other Interesting Results
Blue
These historical mineralized showings have never been drilled. Blue
- Two sub-angular peridotite blocks with 0.55% and 0.68% Cu Eq.
- Several sub-angular to rounded ultramafic blocks ranging from 0.35 to 0.47% Cu Eq
Pogo Northwest
A series of angular felsenmeer blocks of mineralized ultramafics were identified and sampled in this area (Figure 2). These blocks coincide with an electromagnetic conductor and magnetic anomaly aligned with the extension of the Pogo deposit. Large angular mineralized ultramafic blocks returned 0.56%, 0.47% and 0.40% Cu Eq. A mineralized peridotite outcrop just north of the felsenmeers gave 0.44% Cu eq. A few shallow historical drill holes are in the area.
Ground follow-up was conducted at Retty Lake West near historical drill hole A-27 (Figure 3). Metric-scale angular felsenmeer blocks of ultramafics were identified, trending NW-SE and containing up to 10% visible sulfides (pyrrhotite and chalcopyrite) with net-textured sulphides. Assay results range from 0.45 to 0.52% Cu eq. Historical drill hole A-27, 350 meters north-west from the blocks, intersected:
- 0.6% Cu, 0.56% Ni and 0.3% Zn over 0.7 m and 0.25% Cu, 0.24% Ni over 1.04 m.
New Geological Interpretation: High-Potential Corridor
The new geological interpretation at
The northwestern section of this corridor hosts nine mineralized zones originally discovered in the 1950's and extensively drilled in the 80's. These zones contain combined historical estimate of 4.37 million tonnes grading 2.28% Cu Eq * (not NI 43-101 compliant; we believe this estimate is reasonable but cannot be relied upon as current; a qualified person has not done sufficient work to classify the historical estimate as current mineral resources or mineral reserves, and
Each mineralised zone is interpreted to lie within sub-horizontal magmatic conduits that dip at a very low angle to the southeast forming a shallow high potential corridor of at least 1.5 X 15 km. Following and targeting fertile conduits is an important exploration strategy in magmatic Cu-Ni-Co-PGE environments. This newly defined high-potential corridor is the primary focus of CUPANI's exploration efforts this year. A 3,000-4,000 meters drill program will start the first week of
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*a) We believe this estimate is reasonable but cannot be relied upon as current |
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* Cu eq estimates were made using CAD for the copper equivalent calculation with metal prices as of |
QA/QC
The surface grab samples and QAQC samples (479 total) were analyzed by
A total of 22 QAQC samples (blanks and standards OREAS681, 682, 683). Twelve (12) blanks (silica rock) and 10 standards were randomly inserted among the samples sent to ALS Canada for verification and quality control. The reference material comes from
All analytical results for this press release are from surface grab samples.
Qualified Person
The scientific and technical information in this Press Release was verified by
About CUPANI
Forward-Looking Information
Certain of the statements made and information contained herein is "forward-looking information" within the meaning of National Instrument 51-102 – Continuous Disclosure Obligations of the Canadian Securities Administrators. These statements and information are based on facts currently available to the Company and there is no assurance that actual results will meet management's expectations. Forward-looking statements and information may also be identified by such terms as "anticipates", "believes", "targets", "estimates", "plans", "expects", "may", "will", "could" or "would". While the Company considers its assumptions to be reasonable as of the date hereof, forward-looking statements and information are not guarantees of future performance and readers should not place undue importance on such statements as actual events and results may differ materially from those described herein. There can be no assurance that such information will prove to be accurate, as actual results and future events could differ materially from those anticipated in such information. Accordingly, readers should not place undue reliance on forward-looking information. The forward-looking statements in this news release include without limitation, statements with respect to the exploration opportunity related to the
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