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Canada

Cantung Mine

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Summary

Mine TypeOpen Pit & Underground
StatusCare and Maintenance
Commodities
  • Tungsten
Mining Method
  • Truck & Shovel / Loader
  • Longhole stoping
  • Cut & Fill
Backfill type ... Lock
Mine Life... Lock
SnapshotThe Cantung mine was an operating Tungsten mine which shut down and place on Care and maintenance (C&M) in 2015 due heavy debts from its parent corporation North American Tungsten (NATC).

Cantung has come under government ownership (the Canadian government owns the site, and the Government of Northwest Territories holds the mineral rights).

Since November 2015, funding for C&M has been provided by the Canadian government through the Department of Crown-Indigenous Relations and Northern Affairs Canada (DCIRNA).

In 2024, NATC collaborated with DCIRNA to transition C&M activities to the contractor Parsons Canada Inc.

The Extension land use permit (LUP) expires on June 5, 2026. The NATC anticipates either recommencing the New LUP application proceeding, or applying for a broader-scope LUP to continue C&M and advance reclamation work anticipated in 2025 and beyond.

NATC expects to apply for a closure license before the Extension Water Licence expires on January 31, 2027.

Owners

SourceSource
CompanyInterestOwnership
Government of Northwest Territories (operator) 100 % Direct
The Cantung mine is currently under administration and is owned by the Government of the Northwest Territories.

Background

The Cantung mine was previously owned by North American Tungsten Corporation Ltd. On June 9, 2015, Alvarez & Marsal Canada Inc. was appointed as the monitor of North American Tungsten.

Cantung has since come under government ownership, with the Canadian government owning the site and the Government of the Northwest Territories holding the mineral rights.

Contractors

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Deposit type

  • Skarn

Summary:

Cantung is a typical skarn-type deposit, albeit of an unusually large size for a tungsten bearing skarn. As with most skarns, the mineralization is related to a granitic intrusion and its associated intrusive dykes. These intrusive units are believed to have given off reactive fluids that have then come in contact with the overlying reactive Ore Limestone and Swiss Cheese Limestone units.

The two main historic scheelite skarn ore bodies, the Open Pit and E-Zone, are spatially located within the Ore Limestone unit on the upper and lower limbs, respectively, of a recumbent anticline on the west side of the Flat River Syncline.

The major scheelite ore body mined from underground at Cantung historically was the EZone ore body. Since reopening in 2010, the mine has expanded the known extent of the scheelite ore horizon down dip along the lower limb of the recumbent anticline to the south and to the west as well as along the upper limb to the west.

These expanded areas include the West Extension, the Amber zone and Below 3700 elevation level along the lower limb of the fold and the Upper West Extension along the upper limb of the fold. The underground ore zones extend 4,360 ft. along strike, 1,200 ft. down-dip along the lower limb, with some interruption from intrusive sills and dikes, and 200 ft. up dip from the fold hinge along the upper limb.

Throughout most of the underground deposit, three main ore lenses are present: one lens occurs within the Swiss Cheese Limestone, the second lens occurs at the upper contact of the Ore Limestone with the Swiss Cheese Limestone, and the third lens occurs at the lower contact of the Ore Limestone with the Younger Argillite or the granodiorite unit. Intermediate lenses also occur within the Ore Limestone but they tend to be less continuous than either the second or third aforementioned lenses.

The scheelite mineralization in the West Extension and Amber zone is usually fine to medium grained (locally coarse grained), finely to coarsely disseminated and sometimes concentrated in bands, especially within the Swiss Cheese Limestone. These banded concentrations are also observed in the Open Pit Swiss Cheese Limestone ore. Scheelite is usually present in a massive to semi-massive pyrrhotite skarn or a calc-silicate skarn containing abundant pyroxene, garnet and minor pyrrhotite. Both skarn types generally contain chalcopyrite, with some black sphalerite locally. Skarn development in the Ore Limestone and Swiss Cheese Limestone underground is limited by general proximity to the granodiorite intrusive as well as an abundance of fluid transporting fractures and structures. The scheelite mineralization in the Open Pit has been genetically linked by previous researchers to an aplitic dyke and/or quartz vein stockwork that intruded up towards the Open Pit, bringing ore bearing fluids from depth.

Reserves

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Mining Methods

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Heavy Mobile Equipment

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Comminution

Crushers and Mills

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Processing

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Commodity Production

CommodityUnits2015
All production numbers are expressed as concentrate.

Operational metrics

Metrics2015
Tonnes milled 293,709 t

Production Costs

Commodity production costs have not been reported.

Aerial view:

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