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 4

A, B. The sequence of shear structures formation is indicated by brown, black, and yellow colors respectively. C. Copper mineralization on the strike-slip fault surface with the tension evidence. D. Couple of strike-slip faults with an angle of about 70 degrees.

Figure 4. A, B. The sequence of shear structures formation is indicated by brown, black, and yellow colors respectively. C. Copper mineralization on the strike-slip fault surface with the tension evidence. D. Couple of strike-slip faults with an angle of about 70 degrees.