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has been cited by the following article:

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

  AUTHORS: Mahnaz Parvaneh Nejad Shirazi, Fatemeh Dashtaby Jahromi, Mohammad Bahrami

  KEYWORDS: Microfacies; Sedimentary Environments; Faliyan; Shiraz; Zagros

  JOURNAL NAME: Open Journal of Geology, Vol.3 No.2, April 24, 2013

  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.