Abcourt intersects 9.5 g/t Gold over 7.0 metres in channel, including 112.7 g/t over 0.5 metre, more than 650 metres west of the Cartwright Area of the Flordin Project

ROUYN-NORANDA, Quebec, Sept. 25, 2025 (GLOBE NEWSWIRE) -- Abcourt Mines Inc. ("Abcourt" or the "Company") (TSX Venture: ABI) (OTCQB: ABMBF) is pleased to announce its most recent results from the Flordin Cartwright project where two new strippings were completed. These have extended the current mineralized zone to more than 650 metres while identifying new mineralized zones parallel to previously identified zones that had never been exposed or drilled at depth.

The Campaign

Stripping 25-01 presents mineralization parallel to the historic Adam, Horse and Little Joe zones, further north, while being located close to the main access road. This new mineralized zone, which had never been drilled or sampled, identified a gold grade of 1.4 g/t Au over 4.0 metres in Channel No. 1 while remaining open in both directions. The mineralization remains traceable from channel to channel and therefore demonstrates lateral continuity. The new mineralized zone is more silicified than known historical showings; also hematization, which is characteristic of the mineralized zones of the Cartwright area, is absent.

Stripping 25-02 located more than 650 metres west of the Cartwright area contains the Horse and Adam zones. This demonstrates the lateral continuity over at least 700 m of mineralization at the Cartwright area in an area that had not been explored prior to 2025. In addition, Strip 25-02 is located 600 metres SE of hole FL-23-265 which returned 3.9 g/t gold over 19 metres including 14.8 g/t gold over 4 metres (press release dated January 30, 2024). We are now able, thanks to its stripping, to demonstrate the thickening and thinning (socking) phenomena of the mineralized zones over more than 650 metres laterally.

The Methodology Used

The new phase of work made it possible to carry out six channels of approximately 10-15 metres in length on stripping 25-01 as well as 2 on stripping 25-02.

The samples collected are all 0.5 metres long and are connected to each other. Each of the samples averages 6 to 8 cm deep and the channel intersects perpendicularly with the mineralized zones. These zones are oriented approximately east-west and have a sub-vertical dip. The mineralization is associated with significant shear and is composed of pyrite-silica-hematite-rich bands associated with light-coloured alteration (sodium metasomatism). Surface alteration (weathering) of the gossan type (dissolution of pyrites, yellow surface).