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Figure 2. The vertical dykes, mainly spreaded with an East - West trend, reflect a stretch phase with a North - South orientation at the beginning of Eocene and shortly after the formation of the Kaybarkuh body.

Figure 3. Band combination 1/3, 4/7 and 6/4 on Aster satellite image. Yellow and brown colors show the altered units [16].

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 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 6. The general trend of main faults and lineaments in blocks with dimensions of 3 km.

Figure 7. The stress orientation in two time periods according to the observed structures is shown on a Landsat true color (4-2-1) band combination of kaybarkuh region and surrounding.