اخزری، س.، صیرفیان، ع.، وزیریمقدم، ح.، 1394. ریزرخسارهها و مدل رسوبی سازند آسماری (الیگوسن) در شمال غرب روستای دریس (غرب استان فارس) و مقایسه ضخامت، سن و محیط رسوبی با سه برش دیگر در حوضه زاگرس. زمینشناسی نفت ایران، 9: 58ـ43.
آقانباتی، ع.، 1383. زمینشناسی ایران. سازمان زمینشناسی و اکتشاف معدنی، 586 ص.
خسروتهرانی، خ.، 1387. میکروپالئونتولوژی کاربردی، جلد اول: روزنداران. انتشارات دانشگاه تهران، 432 ص.
سازمان جغرافیایی نیروهای مسلح، 1384. نقشه کشور جمهوری اسلامی ایران، مقیاس 1:2000000.
وزیریمقدم، ح.، طاهری، ع.، کیمیاگری، م.، 1390. فرامینیفرا، جنسهای شاخص و دیرینه بومشناسی. انتشارات جهاد دانشگاهی واحد اصفهان، 372 ص.
Adams, T.D., & Bourgeois, F., 1967. Asmari biostratigraphy. Iranian Oil Operating Companies, Geological and Exploration Division, Unpublished Report No. 1074: 1-37.
Akhzari, S., Seyrafian, A., & Vaziri-Moghaddam, H., 2015. Oligocene ramp system (Asmari Formation) in the west of Fars province: Microfacies and sedimentary environment. National Conference on Novel Applied Researches, Urmia, 1: 60-61.
Allahkarampoor Dill, M., Seyrafian, A., & Vaziri-Moghadam, H., 2010. The Asmari Formation, north of the Gachsaran (Dill anticline), southwest Iran, facies analysis, depositional environments and sequence stratigraphy. Carbonate and Evaporites, 25 (2): 145-160.
Bassi, D., Hottinger, L., & Nebelsick, J.H., 2007. Larger foraminifera from the Upper Oligocene of the Venetian area, North-East Italy. Paleontology, 50 (4): 845-868.
Beavingtone-Penney, S.J., & Racey, A., 2004. Ecology of extant nummulitids and other larger benthic foraminifera: applications in palaeonvironmental analysis. Earth Science Reviews, 67 (3): 219-265.
Brandano, M., & Corda, L., 2002. Nutrients, sea level and tectonics: constraints for the facies architecture of a Miocene carbonate ramp in central Italy. Terra Nova, 14 (4): 257-262.
Ehrenberg, S.N., Pickard, N.A.H., Laursen, G.V., Monibi, S., Mossadegh, Z.K., Svana, T.A., Agrawi, A.A.M., Mc Arthur, J.M., & Thirlwall, M.F., 2007. Strontium isotope stratigraphy of the Asmari Formation (Oligocene – Lower Miocene), SW Iran. Journal of Petroleum Geology, 30: 107-128.
Farzipour-Saein, A., Yassaghi, A., Sherkati, S., & Koyi, H., 2009. Basin evolution of the Lurestan region in the Zagros fold and thrust belt, Iran. Journal of Petroleum Geology, 32: 5-19.
Flugel, E., 2010. Microfacies of Carbonate Rocks: Springer, 984 p.
Geel, H., 2000. Recognition of stratigraphic carbonate platform and slope deposits: empirical models based on microfacies analysis of Paleogene deposits in southeastern Spain. Paleogeography, Paleoclimatology, Paleoecology, 1550: 211-238.
Hottinger, L., 1983. Processes determining the distribution of larger foraminifera in space and time. Utrecht Micropaleontological Bulletins, 30: 239-253.
James, G.A., & Wynd, J.G., 1965. Stratigraphic nomenclature of Iranian oil consortium agreement area. American Association of Petroleum Geologists Bulletin, 49 (12): 2182-2245.
Laursen, G.V, Monibi, S., Allan, T.L., Pickard, N.A.H., Hosseiney, A., Vincent, B., Hamon, Y., Van Buchem, F.S.H., Moallemi, A., & Driullion, G., 2009. The Asmari Formation revisited: Changed stratigraphic allocation and new biozonation. First international petroleum conference & exhibition, Shiraz, Iran, 1-5.
MacQillan, H., 1975. Geological compilation map of Kharg - Ganaveh – Kazerun, 1: 250000 scale. Geological and Exploration Division Drawing, sheet No. 20512.
Renema, W., & Troelstra, S.R., 2001. Larger foraminifera distribution on a mesotrophic carbonate shelf in SW Sulawesi (Indonesia). Palaeogeography, Palaeoclimatology, Palaeoecology, 175 (1): 125-146.
Renema, W., 2002. Larger foraminifera as marine environmental indicators. Scripta Geology, 124: 1-260.
Romero, J., Caus, E., & Rossel, J., 2002. A model for the paleoenvironmental distribiution of larger foraminifera based on late Eocene deposit on the margine of the south Pyrenean basin (SE Spain). Palaeogeography, Palaeoclimetology, Palaeoecology, 179: 43-56.
Seyrafian, A., Vaziri-Moghaddam, H., Arzani, N., & Taheri, A., 2011. Facies analysis of the Asmari Formation in central and north-central Zagros basin, southwest Iran. Biostratigraphy, paleoecology and diagenesis. Revista Mexicana de Ciencias Geologicas, 28 (3): 439-458.
Soltanian, N., Seyrafian, A., & Vaziri-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 (2): 167- 180.
Thomas, A.N., 1948. The Asmari limestone of southwest Iran: Report 706, (unpublished).
Van Buchem, F.S.P., Allan, T.L., Laursen, G.V., Lotfpour, M., Moallemi, A., Monibi, S., Motiei, H., Pickard, N.A.H., Tahmasbi, A.R., Vedrenne, V., & Vincent, B., 2010. Regional stratigraphic architecture and reservoir types of the Oligo-Miocene deposits in the Dezful Embayment (Asmari and Pabdeh Formations) SW Iran. Geological Society of London, Special Publication, 329: 219–263.
Vaziri-Moghadam, H., Seyrafian, A., Taheri, A., & Motiei, H., 2010. Oligocene-Miocene ramp system (Asmari Formation) in the NW of Zagros Basin, Iran. Microfacies, paleoenvironment and depositional sequence: Revisita Mexicana de Ciencia Geologicals, 27: 56-71.
Wynd, J.G., 1965. Biofacies of the Iranian consortium-agreement area. Iranian Offshore Oil Company, Tehran, Report No. 1082: 1-80.
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