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).