WORK HISTORY
 
In Jul/2009 ATAC Resources Ltd staked Sten cl 1-20 (YC99501) 300 m to the west and carried out a short prospecting, silt and soil sampling program on the claims. Staked within Sten cl 21-38 (YC995232) in Sep/2009 by ATAC Resources.

In Jul/2010 ATAC Resources staked ST cl 1-431 (YD26901) north, south and east of their existing claim holdings.
 
2012 Work on the Conrad zone consisted of 68 diamond drill holes (total footage not broken out). The company also continued geochemical testing and geological mapping areas located outward from the Conrad – Osiris areas.
 
In 2013, ATAC Resources drilled 4 diamond drill holes (lengths not reported), to expand the strike, length and depth of the zone.
 
In 2014 ATAC Resources collared 4 diamond drill holes (footage not reported) on the Conrad zone. The holes were described as step-out holes designed to test for high grade mineralization and expand the limits of the Lower zone.
 
During the 2015 exploration season ATAC Resources completed one diamond drill hole on the Conrad zone/occurrence. The hole was designed to test for mineralization in the newly designated Lower zone.

GEOLOGY
  
The occurrence area is located in east-central Yukon within an area geologists have referred to as the Rackla belt. The Rackla belt straddles the northern edge of the Selwyn basin, where Neoproterozoic to Paleozoic rocks of the basin are juxtaposed against Paleozoic and older slope and basin rocks of the Ogilvie platform along the Dawson thrust zone. Selwyn basin rocks in the occurrence area are dominated by slope and facies carbonate, clastic rocks and siltstone with significant deep water black shale and chert, whereas the Ogilvie platform is dominated by shallow water platformal carbonate. The occurrence area is bound structurally to the south by the Dawson thrust and to the north by the Kathleen Lake fault. The Dawson thrust is believed to be a reactivated Neoproterozoic normal fault that lies at the northernmost boundary of the Selwyn basin and is generally marked by an abrupt facies change to the Ogilvie platform.
 
The Nadaleen trend consists of a southward-younging sequence of sedimentary rocks that is in fault contact with a large mudstone package north of the Nadaleen fault. The thick mudstone package is an argillaceous mudstone to siltstone with isolated debris flow lenses which Colpron assigns to the Upper Nadaleen assemblage (unit PNu). Sedimentary rock lying south of the Nadaleen fault host the Conrad occurrence and the neighboring Osiris occurrence. The Conrad occurrence is hosted within Tucker’s informal Conrad strata which underlies the Osiris strata. The Conrad stratum consists of silty limestone (unit PNc – Colpron) with siltstone and sandstone as well as large carbonate debris flows interbedded with black shale /siltstone (Unit PNl). Colpron assigns both units to the Lower Nadaleen assemblage. Small, east-west trending, steeply dipping gabbro dykes have been found in the area. The dykes which are mainly found in drill core intersections trend sub-parallel to the Nadaleen fault and range in thickness from 25 cm to 25 m.  Within the Conrad zone the dykes crosscut the limestone and siliciclastic packages.
 
The Conrad zone/occurrence is one of 4 areas of Carlin-type mineralization discovered in 2010-2011 by ATAC Resources. Although gold mineralization was discovered during the 2010 drilling season the formal declaration of Carlin-type mineralization was not made until the spring of 2011 following extensive mineralogical work conducted over the winter of 2010-2011. The Conrad zone consists of a package of carbonates (Conrad Limestone – Tucker) (unit PNc – Colpron) and overlying siltstones to conglomerates (Conrad Siliciclastic – Tucker) (unit PNl – Colpron) that are folded into a broad east-west trending double plunging anticline. The anticline appears to be folded again in the center with the eastern and western limbs curving towards the north. The doubly folded Conrad Limestone and siliciclastic package is in fault contact with the Nonad mudstone unit (unit PNu – Colpron) along the steeply north dipping Nadaleen fault zone. This fault zone ranges up to 50 m wide and is a brittle to ductile cataclasite consisting of fragments of all thee rock units occurring in irregular blocks against one another.

Gold mineralization occurs in both the Conrad Limestone and Conrad siliciclastic rocks, usually within 50 m of the very steeply dipping and often sheared contact. Gold mineralization is accompanied by decalcification and deposition of sooty pyrite, giving mineralized core a darker appearance than unmineralized intersections, although this is very subtle to non-recognizable in siliciclastic rocks. The key factor controlling the distribution of alteration and mineralization is the permeability of the host rocks. According to Tucker (3013) features that control permeability include; primary fluid conduits such as fault and shear zones as well as stylolites, veinlets and fold hinges. Realgar is commonly associated with gold bearing zones, but not all occurrences of realgar have associated gold.
 
To date ATAC Resources has broken the Conrad zone into three separate zones; Upper, Middle and Lower. Carlin type gold mineralization occurs along the stratigraphic contact between Conrad Limestone and an overlying pyritic siltstone cap unit (Conrad Siliciclastics) where the thickest mineralization occurs along the crest of an anticlinal fold. The Upper zone has been continuously traced by shallow drilling over a strike length of 800 m and remains open along strike.
 
The Conrad Middle zone is characterized by strong alteration and gold mineralization within multiple stacked, flat lying bodies proximal to a laterally extensive, near vertical siltstone-limestone contact. Only 300 m of the presently known 800 m long favorable siltstone-limestone contact has been tested and mineralization remains open along strike and depth.
 
Following the 2014 drilling program, ATAC Resources announced the discovery of high-grade gold mineralization at depths of greater than 600 m. The newly discovered high-grade mineralization opens up an entirely new area of exploration. The Lower zone has been defined by two new significant gold intervals that returned 42.67 m of 3.03 g/t gold (624.84 to 667.51 m depth) and 21.71 m of 3.15 g/t gold (697.62 to 719.33 m depth) from diamond drill hole OS-14-230.
 
A 2.3 m trench dug on the Conrad showing uncovered intensely clay altered material. Chip sampling returned an average assay of 14.89 g/t gold over 2.30 m. Rock samples collected from both float and outcrop located around the trench consisted of light to medium grey strongly decalcified limestone with moderate clay alteration and small patches and pockets of realgar mineralization throughout. One rock sample from the area assayed 66.6 g/t gold.