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GoldON Provides Update on Drilling at its West Madsen Gold Project in Ontario's Red Lake Camp

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The eastern boundary of the West Madsen property is a 5 km drive from the Madsen gold mine and mill complex owned by West Red Lake Gold Mines (WRLG)

Victoria, British Columbia--(Newsfile Corp. - October 3, 2024) - GoldON Resources Ltd. (TSXV: GLD) (the "Company") is pleased to provide an update on the exploration drilling program at its 100%-owned West Madsen gold property (the "Property").

Photo 1: Strong to intense epidote-sericite-potassic-hematite alteration, smoky quartz veining and pyrite mineralization commonly ranging 1-3% in a porphyritic granodiorite.

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A total of 1,828.42 metres (m) of diamond drilling was completed over five holes in September.

The objective of the drilling program was threefold:

  1. To follow-up on drill hole WM-21-22 where a granodiorite intrusive body reported 0.16 g/t Au over 195 m including 0.51 g/t Au over 10.90 m.

  2. Investigate a geophysical interpreted fold nose that would provide an important conduit and trap for gold mineralization noted on surface and in the 2021 drill program.

  3. Test the granodiorite intrusive body along strike to the east towards the New Mallen gold occurrence.

Previous drill holes in the target area during 2020 and 2021 were drilled northward within north-dipping stratigraphy. The 2024 drilling campaign aimed at drilling southward, contingent on local topographic relief.

All holes intersected the granodiorite intrusive body with downhole widths up to 57 metres. The granodiorite often displayed strong to intense epidote-sericite-potassic-hematite alteration, smoky quartz veining and pyrite mineralization commonly ranging 1-3% with local areas reaching 5%. Strong crack and seal quartz veining with blebby to disseminated pyrite and chalcopyrite were also noted (Photo 1). The strike length of the granodiorite has now been traced for over 1.25 kilometres.

Photo 2: Strong epidote-sericite alteration in magnetic metasediments with 3-7% fine pyrite. This unit was footwall to the altered and mineralized granodiorite.

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The intense alteration coupled with pyrite mineralization was intersected in all drill holes in lithologies footwall to the granodiorite. Intensely silicified and pervasive epidote-sericite-potassic-hematite alteration of bedded metasediments and mafic volcanic flows with downhole widths up to 19 metres were also intersected. These units had not been intersected in prior drilling programs. Pyrite mineralization was commonly consistent again ranging from 1-3% and locally up to 10%, often along bedding planes appearing to replace magnetite in the metasediments (Photo 2).