Kirkland Lake Discoveries Commences Phase 2 of 10,000-m Drill Program

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Toronto, Ontario--(Newsfile Corp. - January 30, 2024) - Kirkland Lake Discoveries Corp. (TSXV: KLDC) (OTC Pink: KLKLF) ("KLDC or the "Company") is pleased to announce that Phase 2 of its 10,000-m drill campaign at the Kirkland Lake Project has commenced on the Lucky Strike Property. The Company previously completed Phase 1 in September 2023 (see News Release).

The 10,000-m drill program is divided into three phases:

  • Phase 1 consisted of nine holes (2,991 m) drilled on the Goodfish-Kirana property

  • Phase 2 has now commenced and the team will drill approximately 4,000 m at the Hurricane Intrusive Zone, KL East

  • Phase 3 will follow up on Phase 1 and 2 drilling with approximately 3,000 m

"We are excited to drill-test the Hurricane Intrusive Zone with this inaugural program at Lucky Strike," commented Non-Executive Chairman and Founder, Denis Laviolette. "We know that intrusive-related deposits do not happen in isolation and our close proximity to the Upper Beaver deposit, combined with the shared characteristics of the lithologies, alteration, mineralization and geophysics make these drill targets very attractive."

The drill program will initially aim to test the Hurricane Intrusive Zone (Figure 1), which was the subject of prospecting, mapping, and airborne magnetics in 2023. The airborne magnetics program flown in Q2, defined a three-kilometre-long by seven-kilometre-wide anomaly which was further ground-truthed by Kirkland Lake Discoveries in Q3 2023 (Figure 2).


 
Figure 1
Property map showing location of the Hurricane Intrusive Zone at the centre of the KL East Side
 
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Figure 2
Hurricane Intrusive Zone geological map with showings and 2023 grab sample assay results
 
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Ground-truthing identified silicified and intense epidote-altered intermediate intrusions cut by quartz stockwork veinlets and pyrite mineralization at the Whiskey Jack target. Whiskey Jack is situated on an ESE-WSE trending structure on the margin of a magnetic high, interpreted as the contact between mafic volcanics and a syenite intrusion, with a near-vertical structural reading, which may indicate a conduit for the hydrothermal fluids and mineralization in the area. Drilling will test the continuation of this alteration zone at depth.