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Joutel Gold Project

The Joutel Gold Project (“Joutel”) is a high-grade past-producing gold project in Québec, Canada, strategically located along the Casa Berardi-Douay Gold Trend. In December 2024, the Company acquired full ownership and legal title to Joutel following a joint venture restructuring with Agnico Eagle.

Joutel hosts the past-producing Eagle-Telbel mine complex, which operated from 1974 to 1993, producing 1.1 million ounces of gold at an average grade of 6.5 g/t Au during a period of much lower gold prices. The project spans 15.7 km along the Harricana Break (Casa Berardi South), a major gold-bearing structure with strong exploration potential.

The Company has advanced Joutel through extensive data compilation and modern geological modeling. A 3D geological and structural model developed in Q4 2021 identified high-grade gold targets beyond previously mined stopes at Telbel.

A year-long data review and compilation exercise in 2024 integrated historical drill core analysis and digitized data, refining geological and structural controls on gold mineralization. The modern 3D model confirms that the favourable geology hosting the Telbel deposit extends both along strike and at depth, while also identifying new target trends with limited prior drilling.

Joutel spans 39 km², located approximately 70 km southwest of Matagami and 125 km north of Amos. The project is contiguous with the southern boundary of the Douay Gold Project and is accessible via Highway 109, which cuts across the project area.

Joutel straddles the Harricana Break and its eastern continuation, the Joutel Deformation Zone, over 15.7 km. See Figure 1 below for the location of Joutel and the Eagle-Telbel deposits relative to Douay.

Joutel1Figure 1: Plan view on regional base map showing outline of Douay/Joutel/Eagle property outline with Casa Berardi Deformation Zone, Douay resource area and Douay regional targets.

 

For general details on Québec’s infrastructure and mining jurisdiction, refer to the Company’s presentation or the Douay Gold Project page.

 

Gold exploration at Joutel began in 1962, with the first intercepts discovered between 1962 and 1964 through drill testing of magnetic and electromagnetic anomalies. The Eagle-Telbel mining camp, which operated from 1974 to 1993, produced 1.1 million ounces of gold at an average grade of 6.5 g/t Au (Plate 1). Mining at Telbel focused on a single zone between the 600- and 1,000-metre levels, accessed via a drift from the Eagle Mine at approximately 750 metres.


Following the mine’s closure in 1993, work at Joutel shifted to reclamation. For decades, historical drill and stope data remained in paper format until a major digitization effort in 2021 transformed these records into a modern 3D geological model, paving the way for new exploration targeting.

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Plate 1: Eagle-Telbel Mine Complex

After the Eagle-Telbel mine closure in 1993 the Joutel Project shifted to reclamation work. The old analogue drill and stope data remained in paper format until the JV invested approximately C$600k and the better part of 2021 to digitize everything and create a new 3D model

The Joutel Gold Project overlaps the intersection between the northwest-southeast Harricana Deformation Zone and the east-west Joutel Deformation Zone, which collectively mark the southern limit of the CBDZ (Figure 1 and Figure 2).

In the Joutel project area, the uppermost cycle of the Joutel Volcanic Complex, called The Mine Sequence of the Joutel Camp, consists of a thick footwall rhyodacitic to dacitic pyroclastic unit, overlain by interbedded clastic and chemical sedimentary units, fine to coarse felsic pyroclastics, and mafic flows. Within this sequence, a continuous near-vertical horizon termed the Main Iron Carbonate Horizon (MICH), with strong iron carbonate (ankerite) alteration and quartz-carbonate veining, hosted the bulk of past gold production (Figure 2).

In the Joutel mine area and to the northwest, the Mine Sequence is overlain by the Harricana Sedimentary Sequence, which is in fault contact with the Cartwright Mafic Volcanic Sequence to the north.

To the southeast, the Harricana Sedimentary Sequence thins rapidly, and a complex sequence of predominantly felsic tuffs (C-Horizon hanging wall - North Mine Horizon footwall), with various clastic and chemical sediment units, occurs between the Harricana Sedimentary and Cartwright sequences. Two iron carbonate units, North Mine and South Mine Horizons, have also been identified as secondary exploration targets.

All sequences are cut by late major east-northeast to northeast trending Proterozoic diabase dykes.

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Figure 2: Plan view on regional geology base map showing location of the Eagle Mine claim along with additional target trends and >2 g/t Au results from drilling highlighted (red).

The gold mineralization found at Joutel is mostly consistent within its three mains areas, Eagle, Telbel and Eagle West. Gold mineralization exploited at the mines was hosted in steeply dipping to near-vertical semi-massive pyrite-iron carbonate horizons cut by quartz and quartz-dolomite veins and veinlets. Base metal values are low in the mine areas. Quartz-carbonate veinlets in footwall tuffs and carbonate-silica-pyrite alteration zones within the Mine Andesite locally carry significant gold (over 1 g/t), and the top of the Harricana Sedimentary Sequence can also occasionally carry gold.

Both Eagle and Telbel mines are found within a subvertical northwest-southeast striking unit of the Mine Sequence, which hosts several high-grade principal ore shoots plunging at about  55° to  60° to the southeast (Figure 3).

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Figure 3: Longitudinal Section view of the Eagle West, Eagle, and Telbel Mines with mined-out areas in grey and contoured gold grades in g/t Au.

  • Expanded Mineralized Corridor – The 2022/2023 drilling program (7,343 m across three (3) master holes and four (4) wedges) confirmed multiple sub-parallel gold horizons extending beyond historically mined zones at Eagle, defining a broader mineralized corridor with a stratigraphic thickness exceeding 100 metres.
  • Deep Drilling Confirms Gold Below Historical Workings – Drilling at Telbel intersected significant gold mineralization up to 575 m below the lowest mined level, including 3.5 g/t Au over 4.8 m, with higher-grade intervals of 5.2 g/t Au over 2.0 m and 11.1 g/t Au over 0.5 m in semi-massive to massive pyrite (Figure 3).
  • New Exploration Potential Beyond Known Mine Horizon – Broader semi-massive pyrite intervals (up to 100 m thick) with multiple lower-grade gold intercepts suggest mineralization extends beyond the historically mined Eagle-Telbel Horizon, indicating the potential for new gold zones.
  • Untested Depth Potential – The deepest hole (2,242 m) ended in sulfide mineralization with increasing gold grades, suggesting it may have stopped on the edge of a larger sulfide body, highlighting further exploration potential at depth.

Joutel represents a high-grade past producer with significant exploration upside, leveraging modern geological modeling and new drilling to unlock its full potential.