DiscoveryI recently explored a fascinating site for its copper mineralization potential, and the findings are quite promising! This area features gossan bodies rich in various ores and minerals, indicating a significant sub-surface mineralization. Here’s a closer look at what we’ve discovered: Key Observations: 🟢 Copper Oxide Ore: Malachite was found in the area, a green mineral that indicates the presence of copper oxide near the surface. Its vibrant colour is a telltale sign of weathering processes. ⚒️ Copper Sulfide Ore: Traces of chalcopyrite, a copper iron sulfide mineral, were observed. Chalcopyrite is often found deeper in the mineralization profile and suggests potential for more extensive copper deposits below. 🔴 Iron Oxides: Limonite and hematite, along with other associated iron oxide minerals, are present. These minerals are typically formed from the alteration of copper sulfides due to surface oxidation, reinforcing the presence of a weathered gossan body. Mineralization Zones: The gossan body hints at a meaningful mineralization sequence beneath the surface: • Gossan Zone: Surface expression of oxidized massive sulfides minerals. • Leached Zone: Where soluble materials have been removed. • Sulfide Enrichment Zone: Enriched with secondary sulfides formed from leached materials i.e. Chalcocite, covellite, and bornite. • Primary Mineralization Zone: The main zone of hydrothermal deposits containing primary copper sulfides i.e. chalcopyrite. Next Steps in Exploration: To fully evaluate this site’s potential, a systematic exploration program is necessary: 1. Preliminary Geological Assessment: Mapping and sampling to understand surface geology and guide further exploration. 2. Geophysical Surveys: Techniques like magnetic and induced polarization (IP) surveys to reveal subsurface structures and guide drilling. 3. Drilling: Core drilling to sample and analyze subsurface mineralization directly. 4. Resource Estimation: Assessing the quantity and quality of the copper resources.
