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Kenorland and Auranova Announce Completion of Winter Drill Program at the South Uchi Project, Ontario

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Vancouver, British Columbia--(Newsfile Corp. - May 6, 2025) - Kenorland Minerals Ltd. (TSXV: KLD) (OTCQX: KLDCF) (FSE: 3WQ0) ("Kenorland" or the "Company") and Auranova Resources Inc. ("Auranova") are pleased to announce the completion of the 2025 Winter drill program at the South Uchi Project (the "Project"), located in the Red Lake District of Ontario.

2025 Winter Drill Program

The maiden drill program consisted of 27 diamond drill holes totaling 14,363 metres, testing the Papaonga target over an 8km by 3km area, within the large gold-in-till and heavy mineral concentrate (HMC) gold grain anomalies, underlain by bedrock mineralisation consisting of quartz-sulphide veins and disseminated sulphide (see press release dated September 11, 2024). Widely spaced drill fences, roughly 500 metres to greater than 1 kilometre apart were designed to test interpreted structural corridors concealed by deep overburden and Papaonga Lake. Complete assay results are expected to be reported in late Q2 or early Q3 2025.

Figure 1. Plan map showing geology and drill hole locations in the Papaonga target area

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Papaonga Target

This program marks the first-ever drilling at the Papaonga target, following four years of systematic exploration. Prior to this work, no historical drilling or documented gold occurrences had been recorded within the target area. Drilling targeted three principal areas: the sheared margin of the Papaonga diorite, northeast-trending shear zones transecting folded clastic sedimentary rocks with interbedded iron formation, and folded volcanic stratigraphy beneath Papaonga Lake cut by northeast to east-west trending shear zones. Within the diorite, variably developed quartz stockwork to sheeted vein systems were encountered, associated with silica-chlorite alteration, pyrite and trace chalcopyrite mineralisation. The folded clastic sedimentary, iron formation, volcaniclastic and mafic volcanic stratigraphy contain multi-stage veining including widespread early quartz-carbonate veins that are strongly folded and boudinaged associated with pyrite and pyrrhotite mineralisation. Northeast to east-west trending structural corridors, defined by shear zones with strong strain development, host early quartz-carbonate and smoky quartz veins, which are deformed and crosscut by later-stage milky white quartz veins. Alteration consists of moderate silica-sericite-biotite-chlorite assemblages, associated with sulphide mineralisation including arsenopyrite, pyrrhotite, pyrite, and trace chalcopyrite, both within veins and disseminated in the wall rock. Trace, localised visible gold was also observed in association with quartz veining. The multiple vein and sulphide generations are indicative of the long-lived nature of fluid flow and deformation across the Papaonga target area. Although mineralisation is present within the completed holes, it does not necessarily indicate economically significant gold grades.