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A transgression of the Tethys Ocean occurred in east central Iran, like in other areas of the Tethys Ocean, around the Yakhtashian/Bolorian (regional chronostratigraphical units corresponding with the Artinskian/Kungurian of the Early Permian) transition. This led to the development of a carbonate platform that is represented in the Shirgesht area on the northern part of the Tabas Block by the Bagh-e-Vang...
The paleontology and paleoecology of coralline red algal assemblages of Asmari carbonate platform in north-west Zagros basin (Lurestan province) are described. The Asmari Formation was deposited during the Burdigalian to Langhian interval. This Formation unconformably overlies Eocene dolomites of Shahbazan Formation and is conformably underlain by Gachsaran Formation. The thin section analysis of...
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