Microfacies and Sedimentary Environments of the Fahliyan Formation from the Southwest of Iran (Shiraz, Zagros)

DOI: 10.4236/ojg.2013.32008   PDF   HTML   XML   5,530 Downloads   9,442 Views   Citations

Abstract

The Fahliyan Formation is a carbonate sequence of Lower Cretaceous (Berriasian-Hauterivian) in age and was deposited in the Zagros sedimentary basin. This formation is a part of Khami Group and is a reservoir rock in Zagros Basin. This formation was investigated by a detailed petrographic analysis in order to clarify the depositional facies and sedimentary environment in the Kuh-e-Gadvan in Fars Province. Petrographic studies led to the recognition of nine microfacies that were deposited in four facies belts: tidal flat, lagoon, and barrier and shallow open-marine. An absence of turbidite deposits, reefal facies, and gradual facies changes indicate that the Fahliyan Formation was deposited on a carbonate ramp.

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M. Shirazi, F. Jahromi and M. Bahrami, "Microfacies and Sedimentary Environments of the Fahliyan Formation from the Southwest of Iran (Shiraz, Zagros)," Open Journal of Geology, Vol. 3 No. 2, 2013, pp. 49-53. doi: 10.4236/ojg.2013.32008.

Conflicts of Interest

The authors declare no conflicts of interest.

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