Paleoecology of the Asmari Formation in Dashtkuh section In northern of Kaftarak Mountains (East of Shiraz)

Elias Dehghan¹ Reza Safian Boldaji²

1) Master s degree of paleontology and stratigraphy, Technical Department, Caltural and Historical Monicipolity of Shiraz, Iran
2) Engineer in Technical Department, Caltural and Historical Monicipolity of Shiraz, Iran

IOI Code : XYEC-BAHGE
Publication : The 4th International Conference on Engineering and Applied Sciences(4iceasconf.com)
Abstract :
    In this research 167 meters of Asmari Formation sediments in east of Shiraz is studied. Based on microbiostratigraphic study and detecting Lepidocyclina, Operculina, Nummulites assemblage zone, Archaias, Elphidium, Valvulina assemblage zone and Borelis, Meandropsina, Austrotrilina assemblage zone, age of Asmari formation in this area is Oligocene, Lower Miocene. By using of Geochemical and significant parameters of this basin and finally compared with abundance, distribution and the type of wall, we also tried to determine the paleoenvironmental condition of these Formation foraminifers.

Keywords : asmari formation paleoecology oligo miocene zagros iran