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Depositional Environment and Sequence Stratigraphy of Cretaceous Deposits in the Tiran Section, West of Isfahan

The Cretaceous deposits in the Tiran section, west of Isfahan is composed of thick bedded limestones and sandstones. The unconformable succession overlie the Shemshak Formation and underlie the Eocene conglomerate, respectively. The Cretaceous deposits in the Tiran section, west of Isfahan is composed of facies analysis of Cretaceous deposits in the Tiran section indicate that these facies are deposited in the shore line/tidal flat, barrier and open marine Facies belts in a rimmed shelf platform. Sequence stratigraphy analysis led to identification of a 3 order depositional cycle. This depositional sequence related to early rd