TDG Gold Corp. provided a second targeting update focused on the copper-gold-molybdenum ("Cu-Au-Mo") porphyry potential within TDG's 53 square kilometre ("sq.km") Baker Complex, Toodoggone District, B.C. The North Quartz target area is located 4 km west of the Trident target and is bounded by TDG's 100% owned Drybrough target to the north and TDG's former producing Baker Mine to the southwest. North Quartz historically2,3 had only shallow drillholes, all reporting appreciable base metal concentrations.

In 2023, TDG assayed for base metals in historical drillcore from the Baker B-Vein and demonstrated up to 100 metres ("m") of > 1.0 % copper equivalent5 ("CuEq") from near surface. In 2021, TDG completed two diamond drillholes at its 100% owned Drybrough target with both showing anomalous base metals. This more modern drill information has been combined with historical and modern soil geochemistry and geophysics to vector towards a potential porphyry target located beneath North Quartz in a road accessible target area covering at least 5.0 sq.km.

The Baker-North Quartz target area1 is road accessible and located > 1 km from TDG's Baker camp mill and TSF infrastructure. The target area1 is on the north and south flanks of a prominent iron-oxide, gossanous, west-northwest trending ridge adjacent to a regional scale unconformity (now faulted) between the Toodoggone Formation and the Takla Group volcanic rocks; analogous to the ?Kyba-Nelson Red Line' unconformity which hosts deposits in the Golden Triangle area of B.C. The North Quartz target area1 was discovered in the early 1970s and had several generations of ground-based prospecting and sampling campaigns outlining anomalous copper-molybdenum-lead-zinc-gold-silver ("Cu-Mo-Pb-Zn-Au-Ag") concentrations in soil samples, stream sediment samples draining the area, trenches, and shallow drill holes. At least 7 precious and base metal rich quartz-sulphide veins were identified with orientations orthogonal to the Baker A- and B-Veins, suggesting the mineralization may be related, but not directly to the historical Baker Mine.

Historical soils from the North Quartz target area1 outline an open ended 400 m x 450 m multi-element soil anomaly defined by Cu > 100 part per million ("ppm") (ranging from 120-375 ppm); Pb > 100 ppm (ranging from 60-1320 ppm); Zn > 100 ppm (ranging from 100-255 ppm); Mo > 3 ppm (ranging from 3-300 ppm); Ag > 1.5 ppm (ranging from 1.5-9 ppm) and Au >20 parts per billion ("ppb") (ranging from 20-180 ppb). Historical drilling2,3 included completion of 2,930 metres in 28 shallow holes, of which only 23 % was assayed4 (assayed core /total hole length) for precious metals and an even smaller amount for base metals. The length weighted average ("LWA") grade of all the available assayed core is 0.15 % combined Cu+Pb+Zn with numerous intervals showing highly anomalous base and precious metals.

North Quartz is situated along the northeastern contact of the Baker Quartz Feldspar Porphyry stock to the southwest and augite porphyritic andesite and basaltic lava flows of Takla Group to the northeast, adjacent to a regional scale fault that brings Toodoggone volcanics in contact with the Takla on the north valley slope edge. The Toodoggone-Takla contact is a highly prospective horizon for mineralized systems as this contact is thought to be the analogy of the Stuhini-Hazelton contact where prolific deposits have been discovered in the Golden Triangle, on the western flank of the Bowser Basin. High concentrations of base and precious metals in geological materials suggest a base-metal rich system is close by.

Highly altered rocks and mineralized dikes coincident with the ZTEM geophysical responses could be related to an interpreted causative intrusion, appearing as a buried, dome-like high resistivity feature covered with ?blanket-like' zone of lower resistivity. The low resistivity feature is interpreted to be a zone of higher sulphide content associated with the phyllic (quartz-sericite-pyrite) altered cupola of the interpreted intrusion, consistent with field observations. Drillcore host rocks consist of porphyritic augite andesite, aphanitic andesites, lithic tuffs, fragmental volcanics, siltstones, dacites and dykes of varying compositions, most of them strongly altered by silica + potassium feldspar ("K-spar") + epidote + chlorite + pyrite with sulphide mineralization consists of pyrite, sphalerite, galena, and chalcopyrite.

Vein and vein selvage mineralogy is suggestive of a complex hydrothermal environment with dominant assemblages of disseminated chalcopyrite and quartz-chalcopyrite and subordinate magnetite + pyrite assemblages.