Vorschau

Figure 7: Illustrates geological cross sections and drill hole traces of FE-DDH-01A and FE-DDH-01B across the Fierrazo target area with respect to the prograde, retrograde and late porphyry stages of mineralization. It is important to note that the majority of the copper-gold mineralization from the historical drilling is hosted within the calcareous shales and siltstones of the Upper Mara Formation that has a thickness of approximately 70 – 100 meters. The majority of the Ferrobamba has been er