Sadeghi, R., Vaziri-Moghaddam, H. and Taheri, A. (2010) Microfacies and Sedimentary Environment of the Oligocene Sequence (Asmari Formation Moghaddam, H., 2011. Biostratigraphy and Paleo-Ecological Implications in Microfacies of the Asmari Formation (Oligocene) Naura Anticline (Interior Fars of the Zagros Basin) Iran. Carbonates Evaporites, 26, 167-180.

has been cited by the following article:

• TITLE: Sedimentary Environment and Relative Sea Level Changes of the Asmari Formation Deposited in Lurestan Basin, Southwest of Zagros

  AUTHORS: Ava Alizadeh, Davood Jahani, Mohammad Reza Kamali

  KEYWORDS: Asmari Formation, Oligomicene, Microfacies, Sequence Stratigraphic, Lurestan Basin, Southwest of Zagros

  JOURNAL NAME: Open Journal of Geology, Vol.7 No.7, July 18, 2017

  ABSTRACT: Asmari Formation is deposited in the Zagros Foreland basin during Oligo-Miocene time. In the presented research, Sheykh Makan (north of Kabir-Kuh Anticline) section located at Lurestan Basin is studied to achieve an understanding of facies changes, paleoenvironment and also sequence stratigraphic framework (relative sea level changes) of the Asmari Formation. Results of this study revealed that 15 microfacies grouped to four facies belts named as tidal flat, lagoon, barrier and open marine are the main constituents. A homoclinal ramp is determined as the depositional setting of the Asmari Formation. In Sheykh Makan Section, studied interval contains three third-order sequences aging oligmiocene. It overlies gradually shaly Pabdeh Formation and is overlain by evaporitic Gachsaran Formatin.