Filo Mining Corp has announced assay results from holes FSDH055C and FSDH059 from the ongoing drill program at the Filo del Sol Project. Hole FSDH055C is the best hole drilled on the project to date, measured by copper-equivalent multiplied by intercept length, and ended in strong mineralization at almost 1,500m depth. FSDH055C returned 1,337.5m at 1.33% CuEq from 150m, including126.0m at 5.02% CuEq from 728m in Breccia 41, including24.0m at 13.30% CuEq from 728m within the same zoneThe latter intersection included an 8.6m section at 20.25% CuEqThe hole was stopped at a depth of 1,487.5m due to the capacity of the drill, and ended in strong porphyry-style mineralization with the last 21.5m of the hole at 0.93% CuEq (0.62% Cu, 0.41 g/t Au, 0.9 g/t Ag).Filo del Sol is a high-sulphidation epithermal copper-gold-silver deposit associated with one or more large porphyry copper-gold systems. Overlapping mineralizing events combined with weathering effects, including supergene enrichment, have created several different styles of mineralization, including structurally controlled and breccia-hosted gold, manto-style high-grade silver (+/- copper) and high-grade supergene enriched copper within a broader envelope of disseminated, stockwork and breccia-hosted sulphide copper and gold mineralization. This complex geological history has created a heterogeneous orebody which is characterized by zones of very high-grade copper +/- gold +/- silver mineralization within a large envelope of more homogeneous, lower-grade mineralization.The Filo del Sol Project is located in the Atacama Region of Northern Chile and adjacent San Juan province of Argentina, 140 kilometres southeast of the city of Copiapó in Chile and straddles the border between Argentina and Chile.
Filo Mining Corp has announced assay results from holes FSDH055C and FSDH059 from the ongoing drill program at the Filo del Sol Project. Hole FSDH055C is the best hole drilled on the project to date, measured by copper-equivalent multiplied by intercept length, and ended in strong mineralization at almost 1,500m depth. FSDH055C returned 1,337.5m at 1.33% CuEq from 150m, including126.0m at 5.02% CuEq from 728m in Breccia 41, including24.0m at 13.30% CuEq from 728m within the same zoneThe latter intersection included an 8.6m section at 20.25% CuEqThe hole was stopped at a depth of 1,487.5m due to the capacity of the drill, and ended in strong porphyry-style mineralization with the last 21.5m of the hole at 0.93% CuEq (0.62% Cu, 0.41 g/t Au, 0.9 g/t Ag).Filo del Sol is a high-sulphidation epithermal copper-gold-silver deposit associated with one or more large porphyry copper-gold systems. Overlapping mineralizing events combined with weathering effects, including supergene enrichment, have created several different styles of mineralization, including structurally controlled and breccia-hosted gold, manto-style high-grade silver (+/- copper) and high-grade supergene enriched copper within a broader envelope of disseminated, stockwork and breccia-hosted sulphide copper and gold mineralization. This complex geological history has created a heterogeneous orebody which is characterized by zones of very high-grade copper +/- gold +/- silver mineralization within a large envelope of more homogeneous, lower-grade mineralization.The Filo del Sol Project is located in the Atacama Region of Northern Chile and adjacent San Juan province of Argentina, 140 kilometres southeast of the city of Copiapó in Chile and straddles the border between Argentina and Chile.
