A 2003 New Brunswick Government geochemical survey
Strong antimony (Sb) till anomalies in the 95th–100th percentile3
Confirmed polymetallic trench mineralization
2008 soil sampling program documented samples of up to 349ppb Au (Venugopal, 2009)4
Expansion of the land package to 766 hectares
Cambrian felsic volcanic rocks
Metasedimentary units
Northeast-trending fault systems
Structural intersections associated with hydrothermal mineralization
In addition to the presence of elevated Sb values at Hatsfield, a 2008 soil sampling program documented samples of up to 349ppb Au (Venugopal, 2009)3. The gold anomaly is open to the expansion across the Property. The gold anomaly spatially overlaps the Sb anomaly, reinforcing a potential Au-Sb zoned system.
Additionally, a 5-metre channel sample from the Project returned 2.41% Lead (Pb), 0.04% Copper (Cu) and 201 ppm Antimony (Sb) with grab samples returning 4.83% Pb and 0.34 g/t Gold (Au). (Minfile Morell Road)
Given the Project's proximity to the Pike Gold Deposit, the integration of elevated Sb percentile values, a gold-in-soil anomaly, and a 5-metre Pb-Sb mineralized trench supports a compelling exploration thesis targeting a structurally controlled Au-Sb-Pb-Ag hydrothermal system.
Source 4: Venugopal D.V, 2009 Mineral Report of work 476764 – Link
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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