Rackla Gold Property

Osiris Project

Osiris Project


  • Inferred Mineral Resource of 1,685,000 ounces gold at an average grade of 4.23 g/t (in 12.4 Mt), including a pit-constrained Mineral Resource containing 1,055,000 ounces of gold at 4.08 g/t (in 8.0 Mt);
  • Globally competitive discovery cost of CDN $32/oz of gold*; and,
  • Canada's first discoveries of Carlin-type gold mineralization
  • 2010 discovery drill hole at Osiris intersected 65.20 m of 4.65 g/t gold (OS-10-001)
  • 4 zones make up the 12 sq/km Osiris cluster: Conrad, Osiris, Sunrise and Ibis
  • Conrad is the most advanced zone and OS-12-114 intersected 42.93 m of 18.44 g/t gold
  • Mineralization has been traced vertically over 1.2 km between the surface mineralization on the ridge-top of Osiris to the deepest hole (OS-14-230) at Conrad
  • Discovery rate of 21 ounces gold per metre drilled.

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Orion Project

Orion Project

  • Discovery hole at Anubis intersected 8.51 m of 19.85 g/t gold (AN-12-001)
  • Diamond drilling at Orion in 2016 intersected 61.29 m of 2.75 g/t gold (AN-16-010)
  • Trenching and geochemical sampling has outlined a cumulative 8 km strike length of anomalous and potentially mineralized fault structure with well-developed, gold-bearing Carlin-type hydrothermal alteration in adjacent rocks
  • Nine priority exploration targets identified for future drilling at the Anubis, Ana, Hydra, Draco, Dorado, Orion, Zodiac, Columba and Corona showings

2018 Orion Exploration Highlights

  • Gold mineralization associated with the Anubis Fault has now been intersected in diamond drilling over a 2.5 km strike length and to a depth of 540 m;
  • BDO-18-017 intersected 7.61 m of 10.48 g/t gold 380 m down dip of the Anubis discovery outcrop; and,
  • BDO-18-018 returned 10.73 m of 7.20 g/t gold 285 m east of the Anubis discovery.

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Rau Project

Rau Project


  • Since 2007, 22 targets with gold and/or base metal mineralization have been discovered across a 20 km trend at the Rau Property;
  • Targets comprise several distinct styles of intrusive-related mineralization, demonstrating systematic zonation outwards from the Rackla Pluton, which represents one of the proposed hydrothermal fluid sources for the district and may have mineralized porphyry potential;
  • The neighbouring Bobcat target reflects outward fluid flow and the development of gold-copper skarn mineralization. This mineral zonation continues to transition outwards to a gold-silver dominated carbonate-replacement system exemplified by the Tiger Gold Deposit (NPV5% of $106.6 million and an IRR of 34.8% before tax);
  • At the periphery, silver-zinc-lead manto-style mineralization has developed at the Ocelot target, demonstrating distal components of fluid flow.

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