PR Newswire
VANCOUVER, BC, May 23, 2023
VANCOUVER, BC, May 23, 2023 /PRNewswire/ - Capella Minerals Ltd (TSXV: CMIL) (OTCQB: CMILF) (FRA: N7D2) ("Capella" or the "Company") is pleased to provide the following update on exploration activities being undertaken on the Company´s 100%-owned copper-zinc-cobalt ("Cu-Zn-Co") projects in the Hessjøgruva-Kjøli District, Trøndelag Province, central Norway. The Hessjøgruva-Kjøli District consists of the advanced exploration-stage Hessjøgruva VMS Project, the former mining / mineral processing centre at Kongensgruve, and the Kjøli VMS Project (Figure 1), with Hessjøgruva representing the Company´s cornerstone asset in the District.
Figure 1. Locations of the high-grade Cu-Zn-Co Hessjøgruva, Kongensgruve, and Kjøli Projects, Trøndelag Province, central Norway.
Capella is pleased to advise that it has received the key approvals required for initiating diamond drilling at the Hessjøgruva Cu-rich massive sulfide ("VMS") Project on or after July 1, 2023. The issuance of the drill permits is a reflection of the strong community support that the Company has received for advancing the Hessjøgruva project, which has essentially remained idle since the completion of 12,035m / 67 holes of historical diamond drilling in the 1970´s (see Capella´s Canadian National Instrument 43-101 or "NI 43-101" compliant technical report as filed on SEDAR on September 7, 2022; www.sedar.com).
The Hessjøgruva permitting was based on the completion of a minimum of 3,000m / 6 holes of both infill and step-out drilling on the high-grade Hessjøgruva Lens A deposit (Figure 2), one of three main copper mineralized lenses on the property. The upcoming drill program has been designed to assist the Company with its goal of completing a maiden NI 43-101 compliant Mineral Resource Estimate for Hessjøgruva, in addition to providing fresh core for metallurgical testwork and baseline data for initial development studies.
Capella completed an initial 1,412m / 8 hole diamond drill program at the Kjøli Cu-Zn-Co VMS project (Figure 3; Table 1). The eight scout holes were targeted on combined geological and geophysical (electromagnetic and gravimetric) anomalies - considered favourable for the discovery of massive sulfide-type mineralization - in the Guldalsgruva/Rørosmenna area (4 holes), the Kjøli East/Rundhaugen area (2 holes), and the 2km-long Kjøli Deeps target (2 holes, although KJ-008 is a redrill of hole KJ-001 which missed the target due to excessive deviation).
Copper and zinc assays have now been received for drill holes KJ-001 to KJ-007; assays for drill hole KJ-008 (the redrill of KJ-001) at Kjøli Deeps are pending. Locations of completed drill holes and significant intervals returned are indicated below.
Figure 3. Location of scout drill holes at Kjøli.
KJ-004 (Guldalsgruva Sector)
2.9m @ 1.4% Cu from 8.25m downhole (including 0.4m @ 5.3% Cu from 9.5m downhole)
1.2m @ 0.2% Cu + 0.7% Zn from 110.9m downhole
KJ-005 (Rørosmenna Sector)
1m @ 1.5% Zn + 0.4% Cu from 33.35m downhole
0.4m @ 0.8% Cu + 1.4% Zn from 36.4m downhole
KJ-007 (Rørosmenna Sector)
1.8m @ 3.0% Zn + 0.6% Cu from 69.65m downhole
No significant intercepts are reported for drill holes KJ-001, KJ-002 and KJ-006.
Figure 4. Semi-massive chalcopyrite and pyrrhotite in drill hole KJ-004, Guldalsgruva sector. Upper core interval (8.25-9.5m) returned 1.3% Cu, lower core interval (9.5-9.9m) returned 5.3% Cu.
Table 1. Drill hole collars - Kjøli
Drill | Easting | Northing | Altitude | Azimuth | Dip | Depth | Comments |
KJ-001 | 635,373 | 6,973,345 | 1,010 | 140 | -60 | 330.05 | Kjøli Deeps; Excessive |
KJ-002 | 635,729 | 6,973,844 | 967 | 120 | -60 | 248.9 | Kjøli East |
KJ-003 | 635,334 | 6,974,471 | 1,011 | 140 | -60 | 129.1 | Rundhaugen |
KJ-004 | 629,905 | 6,970,380 | 949 | 180 | -60 | 122.55 | Guldalsgruva |
KJ-005 | 628,635 | 6,969,791 | 872 | 0 | -90 | 120.5 | Rørosmenna |
KJ-006 | 629,840 | 6,970,529 | 929 | 180 | -50 | 120.05 | Rørosmenna |
KJ-007 | 628,428 | 6,969,869 | 882 | 160 | -60 | 80.4 | Rørosmenna |
KJ-008 | 635,358 | 6,973,277 | 1,010 | 100 | -60 | 260.55 | Redrill of KJ-001; Assays |
Eric Roth, Capella´s President and CEO commented: "We are very pleased to be announcing the issuance of drill permits for our advanced exploration-stage Hessjøgruva project. In conjunction with exploration efforts being undertaken at the adjacent Kongensgruve and Kjøli projects, we continue to work towards unlocking the resource potential of the broader Hessjøgruva-Kjøli District. I look forward to keeping the market updated as our exploration programs advance."
Capella implemented a Quality Assurance/Quality Control (QA/QC) program to ensure that the logging and processing of the Kjøli drill core was conducted in accordance with NI 43-101 standards and industry best practice. Drill core samples were NQ-sized and were logged, photographed, and marked-up for sampling by Company geologists at a logging facility in the nearby town of Ålen. Core for sampling was then transported to the NGU (Norwegian Geological Survey) core facility in Løkken for cutting with a diamond saw, with one half being dispatched to the analytical laboratory and the other half remaining in storage at the NGU core facility. Sample lengths were typically 1.0 meter but locally adjusted to respect mineralogical contacts and narrower sulfide-bearing zones.
Samples for analysis were then sealed in plastic bags and couriered to MS Analytical in Stensele, Sweden, for sample preparation. All samples were dried and crushed to 70% passing 2mm, with a 250g representative split then being taken and further pulverized to a pulp with 85% passing 75 microns. All pulps were subsequently analyzed for Au, Pt, and Pd (30g fusion with ICP-AES finish; Code FAS-113) plus a multi-element package (4 acid digestion with ICP-AES/MS finish; Code IMS-230). Ore grade intervals of Cu and Zn were further reanalyzed using the ICF-6Cu/6Zn analytical techniques. Internal controls of analytical results were provided through a mix of Certified Reference Materials (standards), duplicates, and blanks inserted by both Capella and MS Analytical in to the analytical sequence.
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