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Trifecta Gold Samples 7.25 g/t Gold from Intrusion-Related System at Rye Project, Yukon and Provides Exploration Update

In This Article:

  • Sheeted veining discovered within hornfels altered sedimentary rocks flanking a granitic intrusion within the Tombstone Gold Belt.

  • Outcrop sampling returned up to 7.25 g/t gold with 240 ppm Bismuth and 5.23 ppm Tellurium.

  • Located near infrastructure 14 km south of the North Canol Highway near Fireweed Metals' Macpass Project.

VANCOUVER, BC / ACCESSWIRE / September 5, 2024 / Trifecta Gold Ltd. (TSXV:TG)(OTCQB:TRRFF) ("Trifecta" or the "Company") is pleased to announce results from its 2024 exploration program at the Rye Project (the "Project"), which consisted of geological mapping, soil sampling and property-wide airborne LiDAR surveying. The Company successfully identified new areas of mineralization within the Itsi pluton and its surrounding hornfels altered sedimentary rocks.

The Rye Project is situated between two Mid-Cretaceous granitic intrusions in the eastern portion of Yukon's Tombstone Gold Belt. It is well located, only 14 km from the North Canol Highway, 15 km from Fireweed Metals Corp.'s Macpass Project, and 95 km from Snowline Gold Corp.'s Valley Gold Deposit. Mapping focused on characterizing vein densities and collecting structural measurements within and adjacent to the Itsi pluton. Results from vein material collected near this contact are tabulated below.

Sample

Description

Au (g/t)

Bi (ppm)

Te (ppm)

D007367

Outcrop sample, quartz vein in granodiorite adjacent to mm-scale sheeted veining (~7/metre)

7.25

240

5.23

D007366

Outcrop sample of arsenopyrite-bearing quartz vein from a zone of sheeted veining mm to 2 cm scale (~6/metre)

1.01

242

16.35

D007387

Arsenopyrite vein in outcrop

3.09

372

11.85

D007373

Grab from top of float train at ridge crest

5.85

1080

6.59

D007370

Grab sample, quartz in float with arsenopyrite

2.72

199.5

3.2

Most of the contact between the Itsi intrusion and the hornfelsed metasediments is covered by large talus fields and glacial colluvium. Intense fracturing and veining have been identified in outcrop within the hornfelsed metasediments, adjacent to intrusive contact, as pictured below. These highly prospective areas have not yet been sampled.

Photo 1

Photo 2

Grid soil sampling in the southern portion of the property better defined an area of overlapping anomalous gold, bismuth and tellurium geochemistry that extends through the mapped hornfels altered sediments to the boundary with the Itsi intrusion.

Finally, a LiDAR ("Light Detection and Ranging") survey was completed over the property to help identify structural features and gain a baseline elevation model, which is necessary for establishing an effective 3-D model for future drilling.