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Brady

Ontario, Canada • 8,811 Hectares

Brady Sudbury
Project

The Brady Sudbury Project includes the Parkin (Golden Pine, Marble Mountain, Black Creek, and Terra Incognita), Fraleck, and River North claim groups, covering a total area of 8,811 ha.

Located on the northeast corner of the Sudbury Structure, the Parkin property is approximately 40 km north of Sudbury, Ontario, with the Fraleck and River North properties situated an additional 6 km to the north.

Mesothermal Lode Gold IOCG Mineralization Nickel-Copper Placer/Till Gold
Brady Sudbury Project Location Map Figure 1. Location map of the Brady Sudbury Project

Geological Setting

Geology

Archean Benny Greenstone Belt

Lode gold showings are hosted by volcanic rocks of the Archean Benny greenstone belt, exposed in the central portion of the Parkin claim group. Quartz-carbonate stringer veins cut altered felsic volcanic rocks within an approximately 150 m wide, northeast-trending shear/fracture system, hosting up to 40% disseminated pyrite with occasional malachite and azurite.

Huronian Sediments & Gabbro

The Galena/Pyrite Hill and Calcite showings are hosted in Huronian sediments cut by northwest-trending structures that regionally extend south along the east side of the Sudbury Structure into the area of IOCG-style gold mineralization at the Scadding Gold Mine. Sulphide mineralization on the River North property is found associated with shears in Huronian sediments and Nipissing-type gabbro.

Major Structural Controls

The River North property is situated along the major regional north-trending Wanapitei Fault, which projects south into the area of the IOCG gold-mineralized Scadding Mine south of Lake Wanapitei. The Vermilion River follows the major northwest-trending Milnet Fault, which in part bounds the western side of the Benny Greenstone Belt.

Sudbury Structure

The Parkin Offset dyke of the Sudbury Structure has been traced to within a short distance of the western edge of the property. Smaller offset dykes have also been identified on the south side of the Parkin property by OGS mapping.

Drill Results & Sampling

Historical Exploration

Golden Pine Drilling

Parkin Claim Group

Historical exploration at Golden Pine identified four subparallel zones — A, A1, B, and C. Drill results include 29.8 g/t Au and 55 g/t Ag over 0.69 m in the "A" Zone, and 6.89 g/t Au over 1.37 m in hole 96-9 from the "A-1" Zone. A channel sample from the "B" Zone returned 14.62 g/t Au and 34.29 g/t Ag over 0.76 m.

29.8 g/t Au over 0.69 m
6.89 g/t Au over 1.37 m
14.62 g/t Au over 0.76 m

2021 Program

Galena/Pyrite Hill

Trenching in 2021 at Galena/Pyrite Hill exposed quartz-carbonate veins with associated pyrite, galena, and minor chalcopyrite. Channel sample results included 3.2 g/t Au, 0.34 g/t Ag, and 0.36 ppm Te over 5.98 m in Channel 5. Two of three 2021 drill holes intersected gold mineralization, including 21.19 g/t Au and 1.4 g/t Ag over 0.68 m in SM-21-03.

21.19 g/t Au over 0.68 m
3.2 g/t Au over 5.98 m

Calcite Showing

Parkin Claim Group

Historical diamond drilling at the Calcite Showing intersected up to 4.25 m of disseminated to massive pyrite in siliceous/cherty intervals, returning 1.54 g/t Au over 1 m and 0.583 g/t Au over 1.16 m. Selected samples were reportedly re-sampled and returned 3.1 g/t Au and 20.57 g/t Au, along with 0.85% Cu, 0.66% Ni, 3% Zn, and 0.07% Co.

20.57 g/t Au
3.1 g/t Au
0.85% Cu

Vermilion River

2015 & 2011 Programs

A 2015 overburden hole program returned nine samples exceeding 10-grain anomalies, with hole 20 yielding 225 grains — a calculated Au value of 6,658 ppb. Approximately 2 km to the north, a 2011 diamond drill hole (BC-11-002) intersected 2.27 g/t Au over 1.0 m within a zone averaging 1.0 g/t Au over 8.9 m.

6,658 ppb Au (225 grains)
1.0 g/t Au over 8.9 m

Where We're Focused

Priority Targets

Golden Pine

Four subparallel lode gold zones within a 150 m-wide shear system. A ~1 km chargeability anomaly remains undrilled.

Galena/Pyrite Hill & Calcite

Post-drilling review recommends follow-up drilling. A southwest-trending anomaly at Calcite appears to intersect the Golden Pine anomaly — an area with no recorded historical diamond drilling.

River North

Inco Gold, Brady Gold, Wanapitei River Copper, and Fraleck/Towers showings along the Wanapitei Fault. Historical grab samples returned up to 3.99 g/t Au and 2.00% Cu.

Vermilion River

Five sites of gold mineralization in till suggest placer potential. Drill hole BC-11-002 averaged 1.0 g/t Au over 8.9 m.