Azimut Provides Update on its Antimony-Gold Drilling Program on the Wabamisk Property, Quebec, Canada

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Exploration Azimut Inc
Exploration Azimut Inc

LONGUEUIL, Quebec, April 10, 2025 (GLOBE NEWSWIRE) -- Azimut Exploration Inc. (“Azimut” or the “Company”) (TSXV: AZM) (OTCQX: AZMTF) is pleased to provide an update on its diamond drilling program on the antimony-gold Fortin Zone at its wholly owned Wabamisk Property (the “Property”) in the Eeyou Istchee James Bay (“James Bay”) region of Quebec.

The initial plan for 5,000 metres was expanded in January, and the program concluded in late March with a total of 51 diamond drill holes completed for 6,211 metres. Antimony sulphides were observed visually in 33 holes. All assay results will be reported as soon as they are received and interpreted. The results will be used to plan an infill and expansion drilling program for early summer.

The Wabamisk drilling program was initiated in late 2024 to follow up on the surface discovery of the Fortin Zone (see press releases of October 29 and December 2, 2024). Partial results from the first 2,090 metres (17 holes completed by the end of 2024) were previously reported (see press release of January 16, 2025). Best intersections included:

  • 1.08% Sb, 0.53 g/t Au over 22.70 m (hole WS24-06)

  • 1.01% Sb, 0.15 g/t Au over 17.85 m (hole WS24-02)

  • 0.87% Sb, 1.41 g/t Au over 9.15 m (hole WS24-13)

  • 1.05% Sb, 0.73 g/t Au over 8.7 m (hole WS24-04)

Due to ongoing supply shortages and exacerbated by trade disputes, the price of antimony has continued rising sharply, recently reaching US$58,000 per tonne in markets outside of China.

HIGHLIGHTS (Figures 1 to 6)

  • Antimony sulphides (mostly stibnite: Sb2S3) have been visually observed in 33 holes. Thirty-one (31) of these holes delineate a mineralized zone with a strike length of least 1.0 kilometre (from WS24-12 to WS24-15). Two (2) holes drilled on the eastern and western extensions of this zone (WS25-22 and WS25-34, respectively) suggest a broader 2.4-kilometre-long prospective corridor. Approximately 300 metres to the south, five (5) holes tested a subparallel trend, mostly delineated by induced polarization anomalies coincident with gold showings.

  • This mineralized system is hosted in an east-west striking subvertical feldspar porphyry intrusive sill and its sheared contacts with metasedimentary rocks (mostly siltstones). To date, 42 holes have intersected the sill over a lateral distance of 2.65 kilometres, and it remains open to the west. Its thickness varies from a few metres to over 90 metres, with a steep dip to the south. So far, the sill has been intercepted vertically down to 140 metres, and a deeper extent is anticipated. The multi-kilometre lateral continuity of the sill could indicate a kilometre-scale vertical depth.

  • The stibnite-bearing system is related to intense quartz veining within the sill and is commonly associated with other sulphides (arsenopyrite, pyrrhotite, pyrite). Sericite is the main alteration mineral, locally accompanied by chlorite, epidote and carbonate. The most abundant mineralization occurs along the southern contact zone with sheared and folded metasedimentary rocks. The northern contact is also mineralized, but drilling to date suggests it is less continuous than at the southern contact. The quartz vein network is mostly subparallel to the east-west schistosity. The rheologic contrast between the brittle porphyry sill and the more ductile metasedimentary rocks appears to be one of the key mineralization controls at the scale of the Fortin Zone.

  • Antimony-rich systems are unusual in Archean settings in Quebec. The mineralized sill on the Property lies along the major tectono-metamorphic boundary separating the volcano-plutonic La Grande Subprovince and the metasedimentary Opinaca Subprovince. This geological environment has already been recognized as prospective for gold, as exemplified by the Eleonore gold deposit. At Wabamisk, the antimony-rich zone may transition to a deeper gold-rich zone. Further drilling will test for antimony-gold vertical zoning, a pattern observed in several deposits around the world.