Tower Stock Gold Property
1. It is not known if the drill hole intervals represent true widths and are therefore being treated as core length intersections.
2. A Qualified Person has not done sufficient work to verify the historical drill core sampling and reported drill core intercepts reported herein.
3. A Qualified Person has not done sufficient work to verify the historical assay results reported by previous operators.
2. A Qualified Person has not done sufficient work to verify the historical drill core sampling and reported drill core intercepts reported herein.
3. A Qualified Person has not done sufficient work to verify the historical assay results reported by previous operators.
Geology
- Gold mineralization occurs in volcanic and sedimentary rocks and syenite intrusive rocks associated with the Tower Mountain Intrusive Complex (TMIC).
- Classified as a syenite-associated disseminated gold deposit type similar to that of deposits in the Kirkland Lake and Malartic gold camps, and the Young-Davidson Mine (Alamos Gold).
- Pyrite is the main sulphide mineral and is generally an indication of anomalous levels of gold.
- Gold mineralization usually controlled by volcanic flows, tuffs and breccias, feldspar porphyries, polymictic conglomerates, syenites and brecciated syenites .
- Pyrite concentrations from trace-1% to a maximum of 15% and sometimes associated with Quartz-carbonate ± tourmaline veinlets carry substantial amount of pyrite, whereas quartz and tourmaline with concentrations of pyrite can form the matrix of intrusive breccias.
Highlights
- Only a small portion of the Tower Stock Gold Project has been explored.
- Historical drill core intercepts outlining high-grade and low-grade gold zones.
- Room to expand on a multitude of targets over 2 km strike length.
- Numerous drill holes ended in gold mineralization.
- Great infrastructure with roads throughout the Project.
- Port city of Thunder Bay only 45 minute drive east of the Project.