Abitibi Metals' Phase II Drill Program: Unveiling the Potential of the B26 Polymetallic Deposit

Abitibi Metals Corp. (CSE:AMQ) (OTCQB:AMQFF) (FSE:FW0) has recently announced the results from its Phase II drill program at the B26 Polymetallic Deposit, highlighting significant mineralization intervals that could potentially expand the resource base and enhance the project's economic viability. This article delves into the key findings from the drill program and explores the implications for the company and the broader mining sector.

The Phase II drill program, comprising 16,500 metres, has focused on testing the Western Plunge and Mid-Level Resource targets at the B26 deposit. The program has yielded promising results, with drill hole 1274-24-338 intersecting an 81.0-metre-long interval of continuous chalcopyrite mineralization from 1,206 to 1,287 metres. This interval, which includes a high-grade zone within the Cu-Au Zone (1,262-1,272 m), demonstrates the deposit's potential for resource expansion and highlights the significance of structural controls and lithological variations in concentrating mineralization.

The presence of chalcopyrite stringers and semi-massive bands associated with quartz veining in the Cu-Au Zone suggests a favorable geological environment for polymetallic mineralization. The continuous mineralization observed in drill hole 1274-24-338 supports the western plunge thesis and indicates the potential for resource expansion along strike and at depth. The deepest intercept in the Project's history, coupled with the recently drilled wedge (1274-24-338-W1), which intercepted 71 metres of chalcopyrite stringer mineralization, further bolsters the Company's confidence in the deposit's potential.

The timing of mineralization at the B26 deposit, relative to regional tectonic events, is crucial for understanding its distribution and grade. The deposit formed during the Mid- to Late-Proterozoic, a period marked by significant tectonic activity in the Abitibi Greenstone Belt. This timing coincides with the waning stages of the Penokean Orogeny, which likely provided the heat and fluids necessary for mineralization. The regional tectonic setting facilitated the formation of large-scale hydrothermal systems that deposited polymetallic minerals, explaining the deposit's size and grade.



The results from the Phase II drill program have significant implications for Abitibi Metals and the broader mining sector. The continuous chalcopyrite mineralization observed in drill hole 1274-24-338 supports the Company's vision of defining a 30-50 million tonne resource at B26. The strong mineralization, composed of chalcopyrite stringers developed against late-tectonic quartz veining, further bolsters the deposit's potential grade and tonnage.

As Abitibi Metals continues to explore the B26 deposit, the growing understanding of its continuity and mineralization patterns will enable a more accurate assessment of the deposit's size and value. The Company's strategic approach to exploration, focusing on structural controls and lithological variations, has proven successful in expanding the resource base and enhancing the project's economic potential.

In conclusion, the results from Abitibi Metals' Phase II drill program at the B26 Polymetallic Deposit have highlighted the significance of structural controls and lithological variations in concentrating mineralization. The continuous chalcopyrite mineralization observed in drill hole 1274-24-338 supports the Company's vision of defining a 30-50 million tonne resource at B26 and underscores the potential for resource expansion along strike and at depth. As the Company continues to explore the deposit, the growing understanding of its continuity and mineralization patterns will enable a more accurate assessment of the deposit's size and value, further enhancing the project's economic viability.