Illustrates the 650 and 200 meter trends of gold and copper mineralization hosted within jasperoid veins within the Ferrobamba limestone formation. The mineralized jasperoid veins are considered as leakage structures from interpreted underlying mineralization situated along the target area.
Illustrates the 650 and 200 meter trends of gold and copper mineralization hosted within jasperoid veins within the Ferrobamba limestone formation. The mineralized jasperoid veins are considered as leakage structures from interpreted underlying mineralization situated along the target area.