The Greywacke Lake Gold Project is located approximately 88 km northeast of La Ronge and 22 km northeast of the community of Missinipe. Road access to the 16,078-hectare (6 claims) project is available via an 11 km access trail that branches southeast from Highway 102. The main project area is comprised of three sub-parallel zones, North, Central and South that are part of the 7 km Wacke Mineralization Trend. The Greywacke North Gold Deposit is located in the North Zone and hosts a historical Mineral Resource Estimate. Other mineralized targets along the Wacke trend include:
Closure Lake and Lyons Zone Showings are located 930m and 1200m along strike to the southwest of the Greywacke North Deposit. These showings are hosted by the same biotite arenite unit that hosts the Greywacke North Deposit. Mineralization consists of a combined 3% pyrite + pyrrhotite and 5% magnetite disseminations and fracture fillings with associated fine-grained (non-visible) gold.
The Hoover Gold Showing is located 3.5 km northeast of the Greywacke North Deposit. The stratiform 5 x 15m gold showing consists of 2 auriferous zones within a sulfide rich biotite arenite unit has hosts up to a combined 5% pyrite + pyrrhotite. Gold occurs as visible grains and intergrowths with the sulfides.
The Wasp Lake Showing is located 2.4 km northeast of the Hoover Gold Showing. This stratiform showing, which is on strike and geologically identical to the Greywacke North Gold Deposit, consists of an auriferous zone within a sulfide-rich biotite arenite with up to 5% pyrite + pyrrhotite and gold that occurs as visible grains and intergrowths with the sulfides.
The Shandy Lake Showing is located 1.5 km NW of the Greywacke North Deposit in a series of metasedimentary rocks that have been intruded by a Berven Lake diorite intrusion. The showing is hosted in a series of 1 to 3m wide subvertical ENE trending sub-parallel shears that form a 50m wide zone of deformation that follows the contact between the diorite and the adjacent lapilli tuffs. Pyrite and associated gold are found as disseminations and fracture fillings in quartz veins within the shear zone.
Greywacke North Gallery
