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Trifecta Gold Outlines a Large, Intrusion-Related Gold Target on its Mt. Hinton Project, Yukon

In This Article:

  • Processing of 2024 geophysical surveys has identified a 3 km long "look-alike" anomaly that marks other Tombstone Gold Belt intrusions in the district

  • Future exploration will prioritize this new target, where Trifecta Gold previously identified granitic boulders on surface

VANCOUVER, BC / ACCESSWIRE / December 2, 2024 / Trifecta Gold Ltd. (TSXV:TG)(OTCQB:TRRFF) ("Trifecta" or the "Company") is pleased to report the results of a 3D inversion of airborne magnetic and Z-Tipper Electromagnetic ("ZTEM") data collected from the Mt. Hinton Project ("Mt. Hinton"). Mt. Hinton is located immediately to the southeast of Hecla Mining's Keno Hill Mine and Mill Complex within the Tombstone Gold Belt ("TGB") of central and eastern Yukon. Processing of the geophysical data, which was collected earlier this year, has confirmed a large, strong resistivity anomaly at the GC target where granitic boulders were discovered in 2024 (Trifecta Gold Announces ZTEM and Magnetic Results from Mt. Hinton Project, Yukon and Describes Ongoing Research Studies). The resistivity feature, which extends along a 3 km axis oriented northwest-southeast, is defined by values in excess of 1235 ohm-m at surface and widening in size at depth. In addition, the resistivity anomaly is spatially associated with a parallel magnetic anomaly (see attached figures). These results are highly suggestive of a buried intrusion in the floor of Granite Creek that may be the driver of mineralization in the district.

Mt. Hinton hosts four major precious metal rich vein trends developed within the Keno Hill Quartzite Formation. Mid- to Late-Cretaceous granitic stocks of the Tombstone and Mayo suites intrude the quartzite sporadically throughout this portion of the TGB. Elsewhere in the belt, Tombstone and Mayo Suite stocks are associated with substantial gold endowments deriving from large arrays of sheeted, sulphide-poor quartz veins hosting native gold. Examples include Snowline Gold Corp.'s Valley deposit, and Sitka Gold Corp.'s RC deposit. Gold mineralization at Mt. Hinton is also thought to be related to this intrusive event, but prior to the 2024 exploration campaign no significant amount of intrusive rock had been identified on the property.

Tombstone and Mayo Suite intrusions commonly generate a contact metamorphic aureole of hornfels, where iron in the form of pyrite is converted to pyrrhotite and generates a concomitant magnetic response; however, pyrite is absent in the Mount Hinton quartzites, and as a result, hornfels mineralogy is expected to be dominated by biotite. The shape and amplitude of the resistivity anomaly at the GC target is highly suggestive of a buried intrusion, while the magnetic response is comparable to responses derived from other Tombstone and Mayo Suite intrusions that host large gold endowments. Combined with the recent discovery of abundant granitic boulders in the valley floor, the Company now considers the GC target to be a high priority drill target.