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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 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 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.
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