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  • Aguilas Project includes 9 Investigation Permits, covering approximately 16,300 hectares in northern Andalucia, Spain 

  • Main targets are major cross cutting fault zones in the Pedroches Batholith, including the Torrubia and Zumanjo Trends


  • IOCG style Cu along the >16 km Northeast oriented Torrubia copper trend

  • Mineral rights cover the >20km Northwest oriented Zumajo Mine Trend with high grade vein/breccia style Pb-Ag (Zn)


  • Torrubia Trend – in May 2019 drilling confirmed wide zones of breccia and Iron Oxide Copper-Gold (IOCG) style mineralization over several kilometers strike length


  • Results included 16m @ 0.30% Cu, 30.5ppm Co, 0.6 g/t Ag, 0.05 g/t Au in drill hole TOR-01, including 0.8m @ 2.65% Cu, 125ppm Co, 3 g/t Ag, 0.004 g/t Au and 0.7m @ 1.85% Cu, 240ppm Co, 2.1 g/t Ag, 0.02 g/t Au, and 0.7m @ 0.55 g/t Au  For complete May 2019 drill results please click here

  • Reconnaissance drill holes completed in November 2019 at the Torrubia North target included seven wide-spaced diamond drill holes spread over approximately 1.6 km of strike with hole spacing from 150 to 600 meters and average hole length of 138 meters. See map below for drill hole locations and collars

  • Drill holes extend the Torrubia Trend and confirm a steep west-dipping zone of multi-stage breccia up to 68 meters thick

  • Several drill holes intersected strongly copper-mineralized clasts within the breccia, providing evidence of an early copper rich stage and exploration potential along the Torrubia structure at depth. (see photos below)

  • High gold values in hole TN-06 are associated with quartz pyrite veins and indicate a separate gold stage

Photos of drill core from the Torrubia North target with examples of breccia clasts containing strong copper mineralization associated with red and black hematite alteration.

a) Drill hole TN-01 showing a chalcopyrite-hematite fragment within a multi-stage, polymictic, quartz-carbonate matrix breccia;

(b) inset – clast with coarse chalcopyrite;

(c) Drill hole TN-02, breccia fragment with strong chalcopyrite and secondary Cu minerals and host within mainly quartz;

(d) drill hole TN-05, with abundant red hematite clasts containing chalcopyrite and secondary Cu, within a largely carbonate matrix.

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