SOMA GOLD EXTENDS VENUS VEIN WITH DRILLING INTERSECTS OF 13.9 g/t Au OVER 7.55m, INCLUDING 48.6 g/t Au OVER 1.45m AND 24.7 g/t Au OVER 1.3m, AT THE CORDERO MINE, EL BAGRE, ANTIOQUIA, COLOMBIA

In This Article:

VANCOUVER, BC, Nov. 12, 2024 /CNW/ - Soma Gold Corp. (TSXV: SOMA) (WKN: A2P4DU) (OTC: SMAGF) (the "Company" or "Soma") is pleased to announce initial results from the 2024 diamond drill program targeting the "Venus Gap" at the Cordero Mine on the Bagre Project in central Colombia (Figure 1). Ten diamond drill holes, totaling 1,476m of underground drilling, were targeted to infill a gap in the historic drilling north of the Venus Vein (see Figures 2 and 3). Previously, mining on the Venus Vein encountered a complex zone of mafic dykes and lower-grade, thin anastomosing quartz veins and was terminated. The drilling results in this release extend the strike of the vein to the northwest and down dip to the northeast.

Highlights include the following drill intercepts:

  • BAZUDDH-24-018: 5.2m at 16.1g/t Au, including 0.8m at 94.3g/t Au

  • RVDDH-23-005: 3.3m at 28.3g/t Au, including 0.5m at 6.3g/t Au

  • RVICDDH-24-018: 1m at 12.5g/t Au

  • RVICDDH-24-021: 1m at 11.2g/t Au, including 0.4m at 27.6g/t Au

  • RVICDDH-24-024: 7.55m at 13.9g/t Au, including 1.3m at 24.7g/t Au and 1.45m at 48.6g/t Au

  • VICDDH-23-006: 3.5m at 10.7g/t Au, including 1m at 21.3g/t Au, 0.85m at 10.7g/t Au, and 0.65m at 9.0g/t Au

The Cordero Deposit is hosted in the El Carmen Stock, comprised of coarse-grained tonalite, diorite, and gabbroic phases. The quartz veins are laminated fault-fill veins within a sinistral brittle-ductile shear zone. They are interpreted as conjugate shears in a steeply-dipping, north-striking regional shear zone. The controlling shear zone also hosts the Los Mangos Deposit, located 2.8 kilometres to the north. The quartz veins within the Cordero Deposit form a series of en echelon segments that consistently step to the right along strike. The veins have been repeatedly reactivated and exhibit three distinct phases of development: early barren quartz veins, sphalerite + galena + pyrite + gold mineralization controlled by microfractures, and brittle fracturing along the vein margins filled with quartz, pyrite, tellurides, and gold. Gold mineralization is associated with the latter two phases of vein development. The final stage of brittle fracturing and micro-breccia is commonly associated with 'bonanza' gold grades. The veins are subsequently crosscut by aphanitic mafic dykes and numerous brittle faults. The brittle faults are generally dextral and offset the quartz veins from <1.0m to 10's of metres. The late brittle faults commonly dismember the mineralized veins into short strike-length segments, the continuity of which is difficult to discern from drill data. The Cordero Deposit is informally divided into five main zones: Athenas, Cordero, Venus, Venus Gap, and Victoria Ramp zones (Figure 2).