Structural controls mineralization in strike-slip fault terminals, case study: Kaybarkuh region in East of Iran

World Journal of Geomatics and Geosciences | Vol 3, Issue 1

Figure 5

The map of main faults which are divided into three generations (G1, G2, and G3) based on field and remote-sensing evidence. Blocks with dimensions of 3 km show the density of lineaments including dykes and minor faults based on total length.

Figure 5. The map of main faults which are divided into three generations (G1, G2, and G3) based on field and remote-sensing evidence. Blocks with dimensions of 3 km show the density of lineaments including dykes and minor faults based on total length.