SOMA GOLD CORP. EXTENDS THE STRIKE LENGTH OF LEVEL 1 BY 68M WITH HIGH-GRADE DRILL INTERCEPTS AT THE CORDERO MINE, EL BAGRE, ANTIOQUIA, COLOMBIA

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VANCOUVER, BC, Sept. 19, 2024 /CNW/ - Soma Gold Corp. (TSXV: SOMA) (WKN: A2P4DU) (OTC: SMAGF) (the "Company" or "Soma") is pleased to announce updated results from its 2024 diamond drill program at the Cordero Mine on the Bagre Project in central Colombia (Figure 1). Results from the first nineteen diamond drill holes in this program were previously reported (press release July 16, 2024), with geochemical analysis pending for the remaining seven holes. This release includes the results from those seven holes, along with twelve additional drill holes.

Cordero Level 1 Diamond Drilling

The Q2/Q3 2024 drilling to date continues to target the up-dip extension of the gold-bearing "Cordero Vein," focusing on delineating the southern extent of Level 1 (Figure 2).  The Cordero Vein has been successfully mined from Level 2 to Level 6. Earlier attempts to develop above Level 2 were hindered by a cross-cutting mafic dyke. The Q2/Q3 drill program aimed to evaluate the western side of the dyke for a continuation of the Cordero Vein, a previously untested target.

Drilling Highlights

  • CORDDH-24-014 1.4m at 2.3 g/t Au incl. 0.4m at 7.9 g/t Au

  • CORDDH-24-019 1.6m at 9.1 g/t Au incl. 1.0m at 14.3 g/t Au

  • CORDDH-24-023 1.2m at 22.3 g/t Au incl. 0.4m at 66.2 g/t Au

  • CORDDH-24-027 1.6m at 5.2 g/t Au incl. 0.55m at 9.2 g/t Au

  • CORDDH-24-029 1.7m at 25.0 g/t Au incl. 0.65m at 35.4 g/t Au and 0.4m at 41.6 g/t Au

  • CORDDH-24-030 1.15m at 8.7 g/t Au incl. 0.5m at 18.2 g/t Au

The Cordero Deposit is hosted in the El Carmen Stock, a polyphase intrusion comprised of coarse-grained tonalite, diorite, and gabbroic phases. Laminated fault-fill quartz veins crosscut the intrusion, forming right-stepping en echelon vein arrays.  The veins are interpreted to be conjugate shear zones that developed within a regional scale, north-striking, sinistral brittle-ductile shear zone.  The controlling shear zone also hosts the Los Mangos Deposit 2.8 km to the north. Mineralized veins exhibit three distinct phases of development: early barren quartz veins, sphalerite--galena--pyrite--gold mineralization controlled by microfractures, and a final phase of brittle fracturing and cataclasis along the margins of the veins filled with quartz--pyrite--tellurides--gold. The final stage of brittle fracturing, micro-breccia, and cataclasis is commonly associated with bonanza gold grades. The veins are subsequently crosscut by aphanitic mafic dykes and numerous, late brittle faults. The late brittle faults typically display dextral strike-slip displacement and offset the quartz veins from <1.0 m 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.