Figure 19. (c): V2a quartz vein; (d): Strongly mineralized quartz vein V2b ( 65.39 g/t)

4.2.2.3 Deformation D3

The D3 deformation is marked by diorite dykes that cut across the tonalite and metasediments. Diorite dykes were also identified and measured in core drill holes (Figure 20). The dykes strike N010 and dip 66° towards SE (Figure 21). The quartz veins associated with the D3 deformation are V3 veins. They are isolated and trends N044 and dips 85° towards the SE (Figure 22 a, b).