SOMA GOLD ANNOUNCES THE COMMENCEMENT OF DRILLING ON PSYCHE 2 COPPER ANOMALY
Figure 2 displays a log-normal index value, combining Cu-Au-Zn-Ni-Co-Mn values, superimposed on the first vertical derivative map. The greater than 95th percentile index values are clustered along the western edge of the soil grid, forming a north-south trending anomaly with a strike length of approximately 4.5 kilometres. This anomaly is located near the Otú Fault and is interpreted to be controlled by associated higher-order structures. The anomalous soil samples also coincide with a prominent magnetic high and a distinct radiometric low (Figures 2 and 3). The cause of the geophysical anomalies is currently unknown due to limited exposure along the length of the anomaly. Geological mapping is underway along the entire length of the anomaly to determine the nature of the underlying bedrock. However, fresh drill core will be critical to resolving the cause of the Copper Anomaly.
The depth extent of the magnetic anomaly underlying the copper anomaly has been constrained by a 3D inversion completed by Convolutions Geoscience (Figure 4). The magnetic anomaly appears to be fault‑bounded along its eastern and western margins and extends to depth. Soil anomalies directly overlie the subcrop extent of the body that forms the magnetic anomaly. The Phase 1 drill program is designed to determine the source of the magnetic and radiometric anomalies in this area.
Phase 1 drilling will target a cluster of soil samples at the northern end of the copper anomaly. Samples in this area comprise some of the most anomalous values of the six index elements within the broader anomaly (see Figures 2 and 3). Phase 1 will consist of four to five drill holes on the first drill pad for a total of approximately 2,000 m of drilling.
Soil sampling has also successfully identified numerous gold anomalies at the Psyche 2 target. The extent and tenor of the copper anomaly represent an exciting new exploration target in the region. Drilling will continue in 2026 at the high-grade gold targets near the
The Otú fault system ("Otú Fault") extends for over 100 km, from Segovia-Remedios in the south to Nechi in the north, where it is buried beneath younger sedimentary overlap sequences. Soma's tenements now cover more than 56 km of this strike length. High-grade gold deposits have been identified along the entire length of the Otú Fault, hosted in brittle-ductile to brittle quartz veins formed during later deformation stages. Throughout the district, quartz veins show orientation patterns consistent with formation in conjugate faults associated with brittle faulting along the Otú Fault. Notable mines along this trend include Segovia-Remedios, La Aurora,
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