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Val-d'Or Mining Exploration Update, Perestroika / Perestroika Ouest Prospects, Eldorado Gold (Quebec) Inc. Options

In This Article:

Val-d'Or, Québec--(Newsfile Corp. - December 19, 2024) - Val-d'Or Mining Corporation (TSXV: VZZ) (the "Company") is pleased to provide an update on exploration activities over the Perestroika and Perestroika Ouest prospects, under option to Eldorado Gold (Quebec) Inc. for the 2024 program.

Property Introduction, Geological and Historical Exploration Overview:

The Perestroika Prospect is located within Courville Township, Quebec, approximately 10 kilometres south of the town of Barraute. The property itself consists of 8 contiguous CDCs covering a total area of 325.43 hectares on NTS map sheet 32C/05 and 32C/06. The adjacent, and contiguous Perestroika Ouest property to the west, consists of five (5) map designated mining title cells totaling 214.18 hectares.

The properties lie along a structural corridor of intense deformation and alteration within the WNW-ESE trending Uniacke Deformation Corridor, inferred as the southeastern strike extension of the prolific Destor-Porcupine Deformation Zone. Previous exploration work located on the Perestroika Prospect established the presence of a gold mineralized trend hosting two (2) historical surface showings, referred to as the "Uniacke Shear" and "Glasnost" gold occurrences. In 2009, drilling by Golden Valley Mines and Royalties Ltd. successfully intersected multiple zones of high-grade gold mineralization associated with this historical gold showings, including drill intersections of 1.15 metres averaging 59.52 g/t Au, including 0.30 metres grading 217 g/t Au in GPS09-01 and 3.50 metres averaging 18.08 g/t Au, including 3.05 metres averaging 20.69 g/t Au in GPS09-02 (GM 54860).

Outcrop exposure on the property is limited to a few known historical gold occurrences and is extrapolated to be underlain by pillowed Mafic Volcanic flows, intercalated with Tuffs of similar composition. These rocks are classified as part of the Landrienne Formation of the Harricana Group. The Landrienne Formation is made up of massive, vesicular, or flow brecciated, pillowed basalt that can be intercalated with felsic lapilli tuffs. Gabbroic sills and porphyritic dikes intrude the mafic volcanic rocks. Only a limited amount of exploration work has been conducted on or proximal to the property, commencing in 1955.

Eldorado Gold (Quebec) Inc. Exploration Work Program Summary:

For the Perestroika and Perestroika Ouest prospects, work completed to date, included vegetation mapping/sampling using spruce tree branches (this is the only work conducted on the Perestroika Ouest Prospect to date), drone imagery, stripping/mapping/channeling sampling over the historical stripped areas ("Uniacke Shear" and "Glasnost"), and diamond drilling.