Douay Project
Emerging Gold Corridor In Northern Québec
The Douay Property provides early-stage exploration exposure within the Abitibi Greenstone Belt, along the Casa Bérardi–Douay–Cameron deformation corridor, approximately 35 km southwest of Matagami.
Exploration Highlights
The Douay Property provides early-stage exploration exposure within the Abitibi Greenstone Belt, along the Casa Bérardi–Douay–Cameron deformation corridor, approximately 35 km southwest of Matagami.
30 Mining Claims
Covering approximately 1,427 hectares across Douay and Vezza townships, in the Abitibi region of Québec.
100% Ownership
Held entirely by Radisson Mining Resources Inc., providing full control over the asset and its future potential.
10,200m Drilled
Across 36 historic holes testing key structural corridors and fault zones, providing baseline geological information for future evaluation.
Best Historic Intercept
5.82 g/t Au over 2.35 m (hole DO-86-16, Harricana Zone), highlighting gold mineralization along established regional trends.
Major Structural Zones
Located along the Douay Fault, Harricana Fault, and Casa Bérardi-Cameron Corridor – key structures hosting multiple gold deposits throughout the Abitibi Belt.
Strategic Optionality
A non-core, early-stage asset providing long-term regional exploration leverage and portfolio optionality within the Abitibi Gold Belt.
In the Heart of a Proven Gold Corridor
- The Douay property lies along the Casa Bérardi–Douay–Cameron structural corridor, known for hosting significant gold systems in the region.
- Nearby deposits include Vezza (13 km east) and Aurvista’s Douay deposit (~6 km to the west).
- The property benefits from proximity to Québec’s mining infrastructure and road access via Highway 109.
Work Achieved
- Between 1985 and 1987, Radisson completed magnetic, EM, resistivity, and IP surveys, followed by 36 drill holes totaling 10,209 metres.
- Drilling identified two major fault zones — the Douay and Harricana deformation corridors — marked by strong sericite, carbonate, and graphitic alteration.
- No further exploration has been conducted since 1987.
- Gold mineralization was intersected in both zones, including 5.82 g/t Au over 2.35 m (hole DO-86-16) within the Harricana deformation system.
Hole DO-86-16, Harricana deformation system (from about 98 m to 102.6 m)
Drilling Results
Main 1985 and 1986 Drilling Results
Hole DO-86-16 brought to light a significant gold intersection grading 5.82 g/t Au over 2.35 metres (including 13.71 g/t over 0.91 metre) in the Harricana Fault zone.
The gold discovery is in the central portion of the property. It occurs in a strongly silicified tuff, which was also identified in hole DO-86-19 at greater depth. Pyrite is the dominant sulphide associated with the alteration, generally with 1% to 5% finely disseminated sulphides (locally 15%).
In the area of the Douay Fault, the work revealed a gold zone with grades reaching 5.49 g/t Au over 0.59 metres. In addition, the drilling intersected two strongly altered shear zones and a pyritic chert horizon along the Douay Fault. Bands mineralized with fine needles of arsenopyrite were also intersected at various levels in several drill holes and were associated with zones of intense tectonism and alteration.
There has been little drilling of the extensions of these mineralized zones and they have not been verified at depth. The association of gold values with the two major faults and the presence of several still untested geophysical targets are good indicators of the property’s potential.
Qualified Person
All scientific and technical data discussed in this document has been prepared by or under the supervision of Yolande Bisson, Eng. MBA,consultant, who acts as a Qualified Person for the Company, as defined by NI 43-101.
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