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 occu ........
