Geology

A Rare Geological Opportunity in Canada

The Casino deposit is one of the country’s most geologically unique and valuable copper-gold systems. Few Canadian deposits rival Casino’s scale and rarity. Its intact supergene-enriched copper-gold zone—laden with critical minerals—owes its existence to geological processes normally erased by successive northern glaciers.

The Casino Deposit

The Casino deposit is a porphyry copper-gold-molybdenum-silver system located in Yukon’s Dawson Range—part of the Tintina Gold Belt in central Yukon. These deposits are formed when mineral-rich fluids rise through fractures in the Earth’s crust, depositing metals as they cool.

This process created one of Canada’s largest undeveloped copper-gold resources, with distinct zones of enriched copper mineralization.

The Geologic Setting

  • The deposit is centred on the 70-million-year-old Patton Porphyry, an east-west trending body of rock
  • This porphyry intrudes older rocks from the Dawson Range Batholith as well as Paleozoic schists and gneisses of the Yukon-Tanana Terrane
  • The intrusion caused brecciation (rock fragmentation) at its northern, southern, and eastern margins, forming rich mineralized zones

Mineralization & Structure

There are three key layers in the deposit:

1.

Leached Cap

Thickness: Top 70 m of the deposit
Mineralization: Weathered zone with oxidized sulphide minerals
Metals: Copper removed; residual gold remains
Notes: Surface weathering from historical leaching processes

2.

Supergene Enrichment Zone

Thickness: Up to 100 m thick
Mineralization: Secondary copper sulphides (higher-grade copper)
Metals: Enriched copper concentration
Notes: Rare in Canada; preserved due to minimal glacial erosion (more common in Chile and U.S. Southwest)

3.

Hypogene Zone

Thickness: Extends more than 600 m below surface
Mineralization: Primary sulphide zone
Metals: Pyrite, chalcopyrite (copper), and molybdenite (molybdenum)
Notes: Represents the long-term production base of the Project

What Makes the Casino Project Unique?

  • It’s a large deposit. The mineralized area stretches about 1.8 km long and 1 km wide.
  • The rich copper layer is well-preserved. Unlike many other sites, the high-grade enrichment zone is intact.
  • The minerals go deep. Valuable metals are found hundreds of metres below the surface.
  • It contains several important metals. The deposit includes copper, gold, molybdenum, and silver, critical for Canada’s economy and clean energy future.
Technical details and drill results are available in the 2022 Feasibility Study (PDF)

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