[1] مطیعی، ه (1372) چینهشناسی زاگرس، انتشارات سازمان زمینشناسی کشور، 536 صفحه.
[2] Adabi, M.H., and Mehmandosti, A.E (2009) Microfacies and geochemistry of the Ilam Formation in the Tang-E-Rashid area, Izeh, S.W. Iran, J. of Asian Earth Sciences, v. 33, p. 267-277.
[3] Adachi, N., Ezaki, Y., and Liu, J (2004) The origins of peloids immediately after the end-permian extinction, Guizhou Province, South China: Sedymentary Geology, v. 164,p. 161-178.
[4] Allen, P.A., and Allen, J.R (2013) Basin Analysis: Principles and Application to Petroleum Play Assessment: Wiely- Blackwell, 655pp.
[5] Armella, C., Cabaleri, N., and Leanza, H.A (2007) Tidally dominated, rimmedshelf facies of the Picún Leufú Formation (Jurassic/Cretaceous boundary) in southwest Gondwana, Neuquén Basin, Argentina. Cretaceous Research, v. 28, p. 961 -979.
[6] Bachmann, M., and Hirisch, F (2006) Lower Cretaceous carbonate platforme of the eastern Levant (Galilee and the Golan Heights), Stratigraphy and second order sea-level change: Cretaceous Research, v. 27, p. 478-512.
[7] Bahamonde, J.R (2007) Marine red staining of a Pennsylvanian carbonate slope: Environmental oceanographic significance. Journal of Sedimentary Research, v. 77, p. 1026-1045.
[8] Bover-Arnal, T., Salas, R., Guimerà, J., and Moreno-Bedmar, J.A (2014) Deep incision on an Aptian carbonate succession indicates major sea-level fall in the Cretaceous. Sedimentology, v. 61, p. 1558–1593.
[9] Bover-Arnal, T., Pascual-Cebrian, E., Skelton, P.W., Gili, E., and Salas, R (2015) Patterns in the distribution of Aptian rudists and corals within a sequence-stratigraphic framework (Maestrat Basin, E Spain). Sedimentary Geology, v. 321, p. 86–104.
[10] Betzler, C., Pawellek, T. Abdullah, M. and Kossler, A (2006) Facies and stratigraphic architecture of the Korallenoolith Formation in North Germany (Lauensteiner Pass, Ith Mountaines): Sedimentary Geology, v. 194, p. 61-75.
[11] Boggs, S.J (2015) Principles of Sedimentology and Stratigraphy (6 th edition): University of Oregon, 660pp.
[12] Booler, (2002) Distribution and geometry of facies and early diagenesis: the key to accommodation space variation and sequence stratigraphy: Upper Cretaceous Congost Carbonate platform, Spanish Pyrenees, Sedimentary Geology, v. 146, p. 225– 247.
[13] Brachert, T.C., Forst, M.H., and Pais, I.J (2001) Lowstand carbonate, highstand sandstone. Journal of Sedimentary Geology, v. 122, p. 155, 1-12.
[14] Cadjenovic, D., Kilibarda, Z., and Radulovic, N (2008) Triassic to Late Jurassic evolution of the Adriatic carbonate platform and Budva Basin, Southern Montenegra: Sedimentary Geology, v. 24, p. 1-17.
[15] Carannante, G., Ruberti, D., Simone, L., and Vigliotti, M (2007) Cenomanian carbonate depositional settings: case histories from the central-southern Apennines (Italy), In: Scott, R., (Eds.), Cretaceous rudist and carbonate platform: environment feedback, SEPM, S.P, v. 87, p. 257.
[16] Carpentier, C., Martin-Garin, B., Lathuilière, B., Gaillard, C., Ferry, S., Hantzpergue, P., and Geister, J (2004) Coral-microbialite reefs in pure carbonate versus mixed carbonate–siliciclastic depositional environments: the example of the Pagny-sur-Meuse section (Upper Jurassic, northeastern France). Facies, v. 50, p. 229-255.
[17] Daizhao, C., Tucker, M.E., Jingquan, Z., and Maosheng J (2002) Carbonate platform evolution: from a bioconstructed platform margin to as shoal system (Devonian, Guilin, South China). Sedimentology, v. 49, p. 737-764.
[18] Della Porta, G., Kenter, J.A.M., Bahamonde, J.R., Immenhauser, A., and Villa, E (2002) Microbial boundstone dominated carbonate slope (Upper Carboniferous, NSpain): microfacies, facies distribution stratal geometry. Facies, v. 49, p. 175–207.
[19] Della Porta, G., Kenter, J.A.M., and Bahamonde, J.R (2003) Depositional facies and stratal geometry of an Upper Carboniferous prograding and aggrading highrelief carbonate platform (Cantabrian Mountains, N Spain). Sedimentology, v. 51, p. 26 7 – 295.
[20] Dill, H.G., Khishigsuren, S., Melcher, F., Bulgamaa, J., Bolorma, Kh., Botz, R., and Schwarz-Schampera, U (2007) Facies-related diagenetic alteration in lacustrine-deltaic red beds of the Paleogene Ergeliin Zoo Formation (Erdene Sum area, S. Gobi, Mongolia). Journal of Sedimentary Geology, v. 181, p. 1–24.
[21] Dunhum, R. J (1962) Classification of carbonate rocks according to depositional texture: in, Ham, W. E. (eds.), Classification of carbonates rocks-A symposium; AAPG, v. 1, p. 108-121.
[22] Eberli, G.P (1987) Calcareous Turbidites and their relationship to sea- level fluctuations and tectonism. in: G. Einsele, W. Ricken, and A. Seilacher (Eds.), Cycles and Events in Stratigraphy. Springer, Verlag, v. 33, p. 340- 359.
[23] El-Azabi, M.H., and El-Araby, A (2007) Depositional framework and sequence stratigraphic aspects of the Coniacian–Santonian mixed siliciclastic/carbonate Matulla sediments in Nezzazat and Ekma blocks, Gulf of Suez, Egypt. Journal of African Earth Sciences, v. 47, p. 179–202
[24] Embry, A.F., and Kloven, J.E (1971) A Late Devonian reef tract on northeastern Banks Island, Northwest Territories, Bulletin Canadian Petroleum Geology, v. 19, p. 730-781.
[25] Fagerstrom, J.A (1991) Reef-building guilds and a checklist for determining guild membership. Coral Reefs, v. 10, p. 47-52.
[26] Flügel, E(2010) Microfacies of Carbonate Rocks Analysis, Interpretation and Application Second Edition. Springer, Berlin-Heidelberg, New York,1006pp.
[27] Fürsich, F., Dhirendra, T., and Pandey. K (2003) Sequence stratigraphic significance of sedimentary cycles and shell concentrations in the Upper Jurassic–Lower Cretaceous of Kachchh, western India. Palaeogeography, Palaeoclimatology, Palaeoecology, v. 193.2, p. 285-309.
[28] Gómez-Pérez, I., Fernádez-Mendiola, P.A., and Garciá-Mondéjar, J (1999) Depositional architecture of a rimmed carbonate platform (Albian, Gorbea, western Pyrenees). Sedimentology, v. 46, p. 337–356.
[29] Haas, J., Götz. A.E., Pálfy, J (2010) Late Triassic to Early Jurassic palaeogeography and eustatic history in the NW Tethyan realm: New insights from sedimentary and organic facies of the Csővör Basin (Hungary). Palaeogeography, Palaeoclimatology, Palaeoecology, v. 291, p. 456–468.
[30] Heldt, M., Bachmann, M., and Lehmann, J (2008) Microfacies, biostratigraphy and geochemistry of the hemipelagic Barremian-Aptian in north central Tunisia: Influence of the OAE 1a on the southern Tethys margin: Palaeos, v. 261, p. 246-260.
[31] Haq, B.U., Hardenbol, J. and Vail, P.R (1987) Chronology of fluctuating sea levels since the Triassic. Science, v. 235.P.1156-1167.
[32] Kenter, J.A.M., Harris, P.M., and Della Porta, G (2005) Steep microbial boundstonedominated platform margins-examples implica- tions. Sedimentary Geology, v. 178, p. 5– 30.
[33] Kenter, J.A.M., Ginsburg, R.N., and Troelstra, S.R (2001) Sea-level driven sedimentation patterns on the slope margin. In: Ginsburg RN, editor. Subsurface geology of a prograding carbonate platform margin, Great Bahama Bank: results of the Bahamas drilling project. Special Publication-SEPM, v. 70, p. 61-100.
[34] Kruse, P.D., and Zhuravlev, A. Yu (2008) Middle–Late Cambrian RankenellaGirvanella reefs of the Mila Formation, northern Iran. Canadian Journal Earth Science, v. 45, p. 619–639.
[35] Laursen, G. V., Monibi, S., Allan, T. L., Pickard, N. A., Hosseiney, A., Vincent, B., Hamon, Y., Van-Buchem, F. S. P., Moallemi, A., and Druillion, G (2009) The Asmari Formation Revisited: Changed Stratigraphic Allocation and New Biozonation, First International Petroleum Conference & Exhibition, Shiraz, EAGE.
[36] Myrow, P.M., Tice, L., Archuleta, B., Clark, B., Taylor, J.F., and Ripperdan, R.L (2004) Flat- pebble conglomerate: its multiple origins and relationship to metrescale depositional cycles. Sedimentology, v. 51, p. 973–996.
[37] Marangon, A., Gattolin, G., Della Porta, G., and Preto, N (2011) The Latemar: A flat-topped, steep fronted platform dominated by microbialites and synsedimentary cements. Sedimentary Geology, v. 240, p. 97-114.
[38] Miall, A.D (2010) The Geology of Stratigraphic Sequences (2 nd Edition): Springer- verlag, 522 pp.
[39] Reijmer, J.J.G., Palmieri, P., and Groen, R (2012) Compositional variations in calciturbidites and calcidebrites in response to sea-level fluctuations (Exuma Sound, Bahamas). Facies, v. 58, p. 493–507.
[40] Tucker, M.E (2011) (4 th edition), Sedimentary Rocks in the Field: John Wiley and Sons, 238pp.
[41] Tucker, M.E., and Wright, V.P (1990) Carbonate Sedimentology. Blackwell, Oxford, 482 pp.
[42] 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., and 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, v. 329, p. 219-263.
[43] Warren, W.J (2000) Dolomite: Occurrence, evolution and economically important association, Earth science review, v. 52, p. 1-81.
[44] Wilmsen, M., and Nagm, E (2012) Depositional environments and facies development of the Cenomanian–Turonian Galala Maghra el Hadida formations of the Southern Galala Plateau (Upper Cretaceous, Eastern Desert, Egypt). Facies, v. 58, p. 229–247.
[45] Wilson, J.L (1975) Carbonate Facies in Geological History. Springer -Verlag, Berlin, 471pp.
)