CSE : TICO  |  FWB : ON8

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Presentation
News Alerts
Presentation

OUR PROJECTS – GOLD & ANTIMONY

Buster Antimony Project

CSE : TICO  |  FWB : ON8

Location:

The region’s geology has provided favorable conditions for both antimony and gold mineralization, specifically in areas where intrusive rocks meet sedimentary layers.

The Buster Project, located in the Clinton Mining Division of British Columbia, is renowned for its potential in both antimony and gold mineralization. This area has a rich history of placer gold production, with thousands of ounces recovered from Stirrup Creek since its discovery in the early 20th century.

*Click to Expand Image

*Click to Expand Image

Geology

The Buster Project is underlain primarily by early Cretaceous sedimentary rocks from the Jackass Mountain Group, including volcanic-rich lithic wackes, shales, and polymict conglomerates.

  • These rocks have been extensively intruded by quartz-feldspar porphyry sills and dykes, which have locally mineralized with fine pyrite, arsenopyrite, and stibnite.

*Click to Expand Images

*Click to Expand Images

Gold & Antimony Mineralization:

  • Antimony mineralization at the Buster Project is closely tied to the presence of stibnite (antimony sulfide), which occurs in narrow veins and disseminations near the contact zones between quartz-feldspar porphyry and argillaceous siltstone.

Gold mineralization in the Buster Project is spatially related to both the intrusions and the fault zones. Gold is often found in veins and veinlets associated with quartz, arsenopyrite, and stibnite.

Historic ~1 km gold-arsenic-in-soil anomaly and ~500 metre antimony anomaly define a large, structurally controlled mineralizing system across multiple target zones

Qualified Person:

The technical information contained in this news release has been reviewed and approved by Graham Giles, P.Geo., VP of Exploration to TICO, who is a Qualified Person as defined under National Instrument 43-101 – Standards of Disclosure for Mineral Projects

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