Lorne plateau

The Bragleenmore Target is a cluster of strong VTEM anomalies coincident with aeromag and gravity anomalies covering 4 square km in a comparable structural setting to the Lagalochan porphyry 8 km to the south.

- 174m @ 0.23% Cu, 0.11g/t Au, 180ppm Mo & 3g/t Ag

- 537m @ 0.18% Cu, 0.1g/t Au, 70ppm Mo & 3g/t Ag

Multiple samples found at Bragleenmore are interpreted as being typical of a marginal k-silicate alteration 300-400m outboard of a central mineralised porphyry Cu stockwork zone

Argyll Metals Limited has signed an exclusive Prospecting Agreement encompassing 12 square km at Bragleenmore

Filtering out lower end noise defines the VTEM anomalies well. The occurrences of outcropping and float potassic altered hornblende-porphyry are all spatially related to the main Bragleenmore VTEM anomaly.
The two isolated anomalies NW of Loch Scammadale are close to epithermal qtz-carb-base metal veinlets and pyritic alteration previously identified.
The anomaly 1.5km south of Bragleenmore is interpreted to be a replacement style sulphidic mineralisation within the local limestone formation.
Bragleenmore samples represent peripheral porphyry Cu mineralization with k-silicate part overprinted by propylitic alteration
As a potential analogy, EM anomalies sourced by 10-15% sulphide stockwork mineralization occur at the Resolution and Collahuasi Cu-Mo porphyry deposits
Geophysical modelling indicates the potential for porphyry related sulphide stockwork mineralization at <150m depth extending to 600m depth underlying Lorne Plateau Volcanic cover