Biostratigraphy of Late Triassic deposits in Central Iranian (Shams abad section in the south of Posht badam Block)

In order to conformity of the sedimentary environment and biological fauna of Late Triassic deposits in each of blocks of the Central Iran, including Lut, Tabas, Posht badam and Yazd blocks, as well as to study the tectonics of the region, were selected sever sections in these blocks, including one section It was studied in the south of Posht badam block in Kerman region, this section is located in the northwest of Kerman city, and Between the Kohbanan and Posht badam faults. The studied section with a thickness of 112 meters is mostly composed of shale, sandstone and limestone. it has many fossils including Bivalves, Sponges, Corals, Bryozoa, Microgastropods and Cephalopods, especially Belemnite, which generally shows the presence of Late Triassic sediments (Norian-Rhaetian) in this area. According to the identified index foraminifera, 8 interval & Concurrence rang biozones Including 5 interval Zone Rectoglandulina tenuis, Triassina hantkeni , Ophtalmidum exigum , Angulodiscus communis, Planiinvoluta regularis and 3 Concurrence rang Zone Turrispirillina minima , Involutina liassica , Duostomina alta , were recognized in the Upper Triassic deposits. Based on the identified biozones, the age of the studied sequences, Late Norian - Early Rhaetian, Middle Rhaetian, Until the end of the Triassic, Late Rhaetian to the beginning of Lias is suggested that they are formation considered equivalent to the members of Howz Khan and Qhadir members from the Nayband Formation in central Iran.