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Dolomitization Mechanism Based on Petrography and Geochemistry in the Shotori Formation (Middle Triassic), Central Iran

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Figure

Figure 1. Major structural-depositional zones of Iran (Stöcklin & Nabavi, 1968) (reload by Nezafati, 2006) and geographical setting of the studied area
Figure 3. The sequence of upper Permian (Pkh), lower and middle Triassic deposits of Sorkh shale (TSo.) and Shotori (TSh.) in Chaharcheshmeh stratigraphic section (north western ward)
Figure 4. Stratigraphy column of the studied area.
Figure 5. (a) Dolomicrite. Type 1 dolomicrite, very fine crystalline, anhedral, Xenotopic (XPL); (b) Dolomicrosparite, Type 2 dolomite, fine to medium crystalline, anhedral to subhedral, Hypi-diotopic (XPL); (c) Dolosparite, type 3 dolomite, medium crystal
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