Document Type : Original Research Paper

Authors

1 Ph.D. Student, Department of Geology, Faculty of Basic Science, Islamic Azad university, Science and Research Branch, Tehran, Iran

2 Assosiate Professor, Payame Noor university, Tehran, Iran

3 Assistant Professor, Department of Petroleum Engineering, Islamic Azad University, Masjed-Soleiman Branch Masjed-Soleiman, Iran

4 Assosiate Professor, Department of Geology, Faculty of Basic Science, Islamic Azad university, Science and Research Branch,Tehran, Iran

Abstract

The Asmari Formation was measured and sampeled in Ghar-e Agha Seyyed at Farsan area in order to determine sedimentary environment based on facies analysis. In the study area, the Asmari Formation has a thickness of 183 m and conformably underlained the Pabdeh Formation. Based on microfacies studies, 8 microfacies were recognized such as:1) Porcelanouse foraminifera – bioclastic – red algal wackestone / packstone, 2) Rotalia grainstone, 3) Bioclastic –red algal grainstone, 4) Red algal – coral boundstone, 5) Red algal wackestone (Floatstone), 6) Red algal –large hyaline foraminifera – intraclast packstone, 7) Red algal – bioclastic  - large hyaline foraminifera  wackestone / packstone, 8) Large hyaline foraminifera packstone. These microfacies represent three facies belts including Inner ramp, Middle ramp and Outer ramp. On the other hand, based on the presence of benthic foraminifera, the age of the Asmari Formation is related to Oligocene (Rupelian – Chatian).

Keywords

References
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