TDG Gold Corp. provided a targeting update from ongoing analysis and interpretation of geophysical data from TDG's 100% owned Mets mining lease located in the Toodoggone District of north-central B.C. Within this news release are the first 3-dimensional ("3D") geophysical renderings of the high-grade Mets A-Zone and its potential northern extension covering a total of 800 metres of the 3,850 m of anomalous trend identified on Mets. Definition of additional drill targets for the remaining anomalous geophysical, geochemical, and structural features at Mets is ongoing.

The historical high-grade, near surface gold ("Au") within the A-Zone at Mets was confirmed by TDG's diamond drilling in 2023 including 20 m of 11.1 grams per tonne ("g/t") Au from 19 m depth, and 8.3 m of 16.4 g/t Au from 51 m depth. The high-grade mineralization appears to be coincident with a parallel west dipping conductive feature and magnetic susceptibility low with a 16-degree plunge to the north. The A-Zone and these geophysical features are interpreted to extend for 800 m and remains open to the north.

The well-understood portion of the Mets A-Zone high-grade Au mineralization is hosted in hydrothermal quartz-barite breccia(s) at/or adjacent to a structurally disrupted lithological contact between the dacite (hanging wall) and andesite (footwall). It can be conceptualized in 3D as a `sheet' of high-grade Au mineralization sub-parallel to the lithological contact which remains open in both directions and at depth. The sheet of mineralization appears to be steeply west dipping, near surface and has a gentle plunge (16°) to the north.

The high-grade mineralized sheet coincides with two geophysical features. Firstly, using a Very Low Frequency Electromagnetic ("VLF-EM") survey, the response is defined by a relative charge density of >12 using the Karous-Hjelt ("KH") filtered 24.8 kHz frequency and is described as a north- trending, plunging anomaly. Secondly, using ground magnetics survey data with the response calibrated by drillhole data, the high-grade sheet coincides with a magnetic susceptibility low, which may represent the destruction of mafic minerals during the course of alteration and mineralization.

Through historical recompilation and modern geophysics, a second alteration/breccia envelope was rediscovered west of the main A-Zone trend. This zone is only partially evaluated by historical drilling, remains open at depth, and shares the same geophysical signatures as the main A-Zone trend. An evaluation of the continuity of this second breccia/alteration zone is ongoing and may represent further dimensionality in endeavors expanding the potential size of the A-Zone.