Work History
 
Staked as part of the Rau cl 1-64 (YC50268) in July, 2006 by ATAC Resources Ltd. The claims are part of the larger Rackla Gold Project, which were staked following the discovery of gold mineralization in 2008 at the company’s Tiger occurrence (MINFILE occurrence 106D 098) 575 m to the west of the Cub occurrence. In 2008, the company performed a helicopter-borne magnetic and variable-time domain electromagnetic survey, soil sampling and prospecting over the newly staked area, including Cub occurrence.
 
ATAC Resources carried out follow-up prospecting over the Cub occurrence area in 2009, 2010 and 2017.

Regional & Property Geology

The occurrence lies with the Rau Trend between the Dawson and Kathleen Lakes thrusts, which form part of a band of regional-scale thrust faults that imbricate rocks of Mackenzie Platform and Selwyn Basin. The occurrence area lies on the western margin of ancestral North America and is underlain primarily by shallow water carbonate and clastic sediment rocks of the Mid-Proterozoic to Paleozoic Mackenzie Platform and the Neo-Proterozoic to Paleozoic, regionally metamorphosed Selwyn Basin clastic rocks. These rocks formed a fault-bounded sediment package which was thrust northeasterly during Jurassic to Cretaceous times by the Dawson and Kathleen Lakes thrust faults onto predominantly Proterozoic rocks. Following thrust faulting, Late Cretaceous (94-90 million years) intermediate to felsic plutons of the Tombstone Suite were emplaced (Mortensen et al., 2000). A second compressional orogenic event around 65 million years saw the emplacement of felsic intrusives assigned to the McQuesten Suite.
 
Other than the immediate area surrounding the Tiger deposit (MINFILE occurrence 106D 098), the occurrence area has not been geologically mapped in detail. ATAC Resources (AR 096936) has mapped 3 main units in the area comprising the Rau Trend:
1. Cambrian to Ordovician massive, grey dolostone,
2. Ordovician and/or Silurian bedded, grey and buff silty limestone and massive white limestone, and
3. Silurian to Devonian thick, bedded dolostone and limestone.

The company has assigned all three units to the Cambrian to Devonian Bouvette Formation. Colpron’s 2013 geological map generally supports this interpretation; however it uses slightly different age dates and doesn’t include the oldest rocks (Cambrian to Ordovician dolostones) within the Bouvette formation.

Thin volcaniclastic horizons assigned to the Ordovician Marmot Formation are interbedded with the Ordovician and/or Silurian limestones and a narrow sliver of Mid-Proterozoic Fifteen Mile Group dolostone underlies the Bouvette Formation rocks to the southwest. Devonian and Mississippian Earn Group comprised of black shale and chert bounds the Bouvette Formation to the south east and north in the southern half of the Rau Trend property.

Mineralization at the Rau Trend varies and consists mainly of: sediment-hosted replacement-style Au; structurally hosted Ag-Pb-Zn; skarns; Au-bearing quartz veins; and transported gossans/unknown deposit style (AR 096936).

Mineralization & Results

The Cub occurrence is a 110 m wide by 250 m long area of anomalous float discovered in 2009 by ATAC Resources that coincides with a high bismuth-in-soil anomaly (>200 ppm Bi).

Float samples taken in 2009 and 2010 by ATAC Resources typically returned anomalous bismuth with the highest samples ranging from 1645 ppm Bi to 6160 ppm Bi. Some rock samples also returned gold values of up to 1.15 g/t Au. A different float sample taken on the southeastern edge returned 18.15 g.t Ag, 4630 ppm Pb and >1% Zn. Prospecting was also performed in 2017.

Assessment Reports that overlap occurrence