منابع
[1] رحیمپور بناب، ح (1389) سنگ‌شناسی کربناته با نگرشی بر کیفیت مخزنی، انتشارات دانشگاه تهران، 554 ص.
[2] زارع، م (1382) بررسی محیط رسوبی و دیاژنتیکی سازند فهلیان در چاه‌های آغاجاری 140 و منصوری 6، پایاننامه کارشناسیارشد، دانشگاه تهران، 127ص.
[3] سوری، ل.، رحیم پوربناب، ح.، کاوسی، م, ع (1385) نقش گسل ایذه در تعیین مدل رسوبی سازند فهلیان در جنوب خاوری ایذه و فروافتادگی دزفول شمالی، دهمین همایش انجمن زمینشناسی ایران، دانشگاه تربیت مدرس.
[4] لاسمی، ی.، نورافکن، خ (1384) رخساره‌ها و محیط رسوبی سازند فهلیان در میدان نفتی دارخوین، جنوب باختر ایران، مجموعه مقالات نهمین همایش انجمن زمینشناسی ایران، دانشگاه تربیت معلم.
[5] محمدخانی، ح (1382) بررسی محیط رسوبی و چینه‌نگاری سکانسی سازند فهلیان در میدان‌های نفتی خویز و رگ سفید در بخش جنوبی دزفول، پایاننامه کارشناسیارشد، دانشگاه تربیت معلم، 68 ص.
[6] مطیعی، ه (1372)زمینشناسی ایران، چینهشناسی زاگرس، انتشارات سازمان زمینشناسی کشور، 536 ص.
[7] Abyat, A., Baghbani, D., Afghah, M., Kohansal Ghadimvand, N., Feghi, A (2012) Microbiostratigraphy and Lithostratigraphy of Fahliyan and Gadvan Formations in Kuh-e-Surmeh (Zagros Basin, Southwest Iran) advances in environmental biology, 6(12): 3078 3086.
[8] Adabi, M.H., Salehi, M.A., Ghobeishavi, A (2010) Depositional environment, sequence stratigraphy and geochemistry of Lower Cretaceous carbonates (Fahliyan Foemation), south–west Iran: Journal of Asian Earth Sciences, v. 39, p. 148–160.
[9] Ahmad, A.H.M., Bhat, G.M.M., Azim Khan, H (2006) Depositional environments and diagenesis of the kuldhar and Keera Dome carbonates (Late Bathonian–Early Callovian) of Western India. Journal of Asian Earth Sciences, 27, 765–778.
[10] Alsharhan, A.S., Nairn, A.E.M (1988) A review of the Cretaceous Formations in the Arabian Peninsula and the Gulf: Part II. Mid-Cretaceous (Wasia Group) Stratigraphy and Paleogeography. Journal of Petroleum Geology, U.K., v.11, pp. 89-112.
[11] Amodio, S (2006) Foraminifera diversity changes and paleoenvirenmental analysis: the lower Cretaceous shallow–water carbonate of Sanlorenzello, companion Apennines, southern Italy, Facies, 52:53-67.
[12] Amouthor, J.E., Fridman, G.M (1992) Early to late diagenetic dolomitization of platform carbonate: Lower Ordovician, Ellenbuger Group, Permian Basin, West Texas, Journal of Sedimentary Petrology, v. 62, p. 131–143.
[13] Armella, C., Cabaleri, N. and Leanza, H (2007) Tidally dominanted, rimmed-shelf facies of the Picu Leufu Formation (Jurassic/Cretaceous boundary) in Southwest Gondowana, Neuquen Basin, Argentina, Cretaceous Resarch, 28, p. 961–979.
[14] Bachmann, M., Hairsch, F (2006) Lower Cretaceous carbonate platform of the Eastern Levant (Galilee and the Golan Heights): stratigraphy and second-order sea-level change: Cretaceous Research, no. 27, p. 487 512.
[15] Bathurst, R.G.C (1975) Carbonate Sediments and their Diagenesis, Development in sedimentology, v. 12, Elsevier, Amesterdam, 658p.
[16] Beavington-Penney, S.J., Nadin, P., Wright, V.P (2008) Clarke E.d., McQuilken J. & Bailey H.W., “Reservoir quality variation on an eocene carbonate ramp”, El Garia Formation, offshore Tunisia: Structural control of burial corrosion and dolomitisation, Sedimentary Geology., Vol. 209, PP. 42–57.
[17] Bordenave, M.L., Burwood, R (1995) The Albian Kazhdumi formation of the Dezful Embayment, Iran: One of the Most efficient Petroleum generation systems. Spriger Verlag pub, 342pp.
[18] Burchette, T.P., Wright, V.P (1992) Carbonate ramp depositional systems. Sedimentary Geology 79, p3–57.
[19] Butler, I.B., Rickard, D (2000) Framboidal pyrite formation via the oxidation of iron (II) monosulfide by hydrogen sulphide: Geochimica et Cosmochimica Acta, v. 64, p. 2665-2672.
[20] Buxton, M.W.N., Pedley, H.M (1989) A standardized model for Tethyan Tertiary carbonates ramps: Geological Society. London, Special Publication, 149, 746-748.
[21] Choquette P.W., Pray L.C (1970) Geologic nomenclature and classification of porosity in sedimentary carbonates, AAPG Bulletin., Vol. 54, PP. 207–250.
[22] Dorobeck, S.L., Read, J.F (1986) Sedimentology and basin evolution of the Siluro-Devonian Helderberg Group, central Appalachians. Journal of Sedimentary Petrology, 56: 601–613.
[23] Dunham, R.J (1962) Classification of carbonate rocks according to depositional texture. AAPG Memoir 1, p. 108–121.
[24] Dunham, R.J (1970) Keystone vugs in carbonate beach deposits [abs.]: American Association of Petroleum Geologists Bulletin, v.54, p.845.
[25] Eichenseer, H.T., Walgenzitz, F.R., Biondi, P.J (1999) Stratigraphy Control on Facies and Diagenesis of Dolomitized Oolitic Siliciclastic Ramp Sequence (Pinda Group, Albian Offshore, Angola) AAPG, Bulletin, v.83 no. 11, P. 1729–1758.
[26] Esteban, M., Taberner C (2003) Secondary porosity development during late burial in carbonate reservoirs as a result of mixing and/or cooling of brines, Journal of Geochemical Exploration., v. 78-79, PP. 355–359.
[27] Embry, A.F., Klovan, J.E (1971) A Late Devonian reef tract on northeastern Banks Island: Can. Journal of Petroleum Geology, v.19, 51p.
[28] Emery, D., Meyers, K.J (1996) Sequence Stratigraphy. Blackwell Science Ltd, Oxford, v 297 pp.
[29] 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 (1), 5–19.
[30] Flugel, E (2010) Microfacies of carbonate rocks. Analysis, interpretation and application: Springer, Berlin Heidelberg, New York, 144p.
[31] Given, R.K., Wilkinson, B.H (1985) Kinetic control of morphology, composition and mineralogy of abiotic sedimentary carbonate. Journal of Sedimentary Petrology, v. 55, p. 109–119.
[32] Goldhaber M.B (2004) Sulfur-rich sediments”, In: Mackenzie F.T. (Ed.), Sediments, Diagenesis, and Sedimentary Rocks,Treatise on Geochemistry, Elsevier, Amsterdam, pp. 257–288.
[33] Hood S.D., Nelson C.S., Kamp P.J.J (2004) Burial dolomitisation in a non tropical carbonate petroleum reservoir: the Oligocene Tikorangi Formation, Taranaki Basin, New Zealand, Sedimentary Geology., v. 172, PP. 117–138.
[34] Jamalian, M., Adabi, M.H., Moussavi, M.R., Sadeghi, A., Baghbani, D., Ariyafar, B (2011) Facies characteristic and paleoenvironmental reconstruction of the Fahliyan Formation, Lower Cretaceous, in the Kuh-e Siah area, Zagros Basin, southern Iran, Facies, 57 (1). 101-122.
[35] James, G.A., Wynd, J.G (1965) Stratigraphic nomenclature of Iranian oil consortium agreement area. American Association of Petroleum Geologist, Bulletin 49, 2182–2245.
[36] Koop, W., Stoneley, R (1982) Subsidence History of the Middle East Zagros Basin, Permian to Recent: Philosophical Transactions, Royal Society of London, A305, p. 149–168.
[37] Kamali, M.R., Lemon, N.M., Apak, S.N (1995) Prosity generation and reservoir potential of Ouldburra Formation carbonate Officer Basin, South Australia, Association for Petroleum and Explosives Administration, p. 106 – 120.
[38] Laporte, L.F (1969) Recognition of a transgressive carbonate sequence within an epeiric sea: Helderberg Group (Lower Devonian) of New York State. In: G.M. Friedman (Editor), Depositional Environments in Carbonate Rocks. A Symposium: Society of Economic Paleontologists and Mineralogists special. p, 14: 98–119.
[39] Lawrenc, M.J.F (1994) Conceptual model for early diagenetic chert and dolomite, Amuri Limestone Group, Noeth easternsouth Island, New Zealand, Jour. Journal of Sedimentary Petrology. v. 41, p. 479–498.
[40] Lee, M.R., Harwood, G.M (1989) Dolomite calcitization and cemen zonation related to uplift of the Raisby Formation (Zechstein carbonate). Northeast England. Sedimentary Geology. 65, 285–305.
[41] Lee, Y.I., Friedman, G.M (1987) Deep-Burial Dolomitization in the Lower Ordovicia Ellenburger Group Carbonate in West Texas and Southeastern New Mexico, Journal of Sedimentary Petrology, 57, 544–557.
[42] Longman, M.W (1980) Carbonate diagenetic textures from near-surface diagenetic environments. American Association of Petroleum Geologists, Bulletin., 64, 461–487.
[43] Machel, H.M (2004) Concepts and models of dolomitization: a critical reappraisal. In: Braithwaite, C.J.R., Rizzi, G., Darke, G. (Eds), The Geometry and petrogenesis of dolomite hydrocarbon reservoirs, Geological Society, London, Special Publication, 235, 7–63.
[44] Madi, A., Bourque, P.A., Mamet, B.L (1996) Depth – related Ecological Zonation of a Carboniferous Carbonate Ramp, Upper Visean of Bechar Basin, Western Algeria, Facies,Erlangen, No.35., P. 59–80.
[45] Maleki, S., Lasemi, Y (2011) Sedimentary Environment Sequence Stratigraphy of the Fahliyan Formation in Assaluyeh (Bidkhon) and Khartang Sections, Southwest Iran. Journal of Basic and Applied Scientific Research., 1(12)2641-2647
[46] Middletone, G.V (1973) Johhanes Walther΄s law of correlation of facies, Bull. Geol. Soc. Of Am, V. 84, P. 979–988.
[47] Miller, J (1988) Cathodoluminescence microscopy. In: Thchniques in Sedimentology (Ed.by M.E.Tucker). pp. 174–190. Blackwells. Oxford.
[48] Moore, C.H (2001) Carbonate reservoir porosity evolution and diagenesis in a sequence stratigraphic framework. Elsevier, Amsterdam, 444 p.
[49] Morrow, D.W (1982) Diagenesis, dolomites, part two: dolomitization models and ancient dolostones. Geoscience Canada 9: 95–107.
[50] Murris, R.J (1980) Middle East: stratigraphic evolution and oil habitat. American Association of Petroleum Geologists, Bulletin 64: 597–618
[51] Purser, B.H., Tucker, M.E., & Zenger, D.H (1994) Problems, progress and future research concerning dolomites and dolomitisation, In: Purser, B., Tucker, M., Zenger, D. (Eds.), Dolomites, A Volume in Honour of Dolomieu, Blackwell, PP. 3–20.
[52] Read, J.F (1980) Carbonate ramp to basin transitions and foreland basin evolution, Middle Ordovician, Virginia Appalachians. American Association of Petroleum Geologists, Bulletin, 64: 1575–1612.
[53] Read, J.F (1985) Carbonate platform facies models. American Association of Petroleum Geologists, Bulletin, 69: 1–21.
[54] Sanders, D (2001) Burrow-mediated carbonate dissolution in rudist biostromes (Aurisina, Italy), implications for taphonomy in tropical, shallow subtidal arbonate environments. Palaeogeography, Palaeoclimatology, Palaeoecology, 168, 39–74.
[55] Scholle, P.A., Ulmer-Scholle, D.S (2003) A Color Guide to the Petrography of Carbonate Rocks: Grains, Textures, Porosity, Diagenesis. American Association of Petroleum Geologists Bulletin, Memoir, v. 77, USA, 474p.
[56] Setudehnia, A (1978) The Mesozoic sequence in southwest Iran and adjacent areas. Journal of Petroleum Geology 1: 3–42.
[57] Shakeri, A., Parham, S (2013) Reservoir Characterization and Quality Controlling Factors of the Fahliyan Formation Located in Southwest Iran. Journal of Sciences, Islamic Republic of Iran 24(2): 135-148
[58] Shebl, H.T., Alsharhan, A.S (1994) Sedimentary facies and hydrocarbon potential of Berriasian- Hauterivian carbonates in centralArabia. In Micropalaeontology and Hydrocarbon Exploration in the Middle East . Edited by M.D. Simmons. Chapman & Hall, London. pp.159-175.
[59] Sherkati, S., Letouzey, J (2004) Variation of structural style and basin evolution in the central Zagros (Izeh zone and Dezful Embayment), Iran. Marin and Petroleum Geology 21, 535–554.
[60] Sibley, D.F., Gregg, J.M (1987) Classification of Dolomite Rock Textures: Journal of Sedimentary Petrology, no.57, p. 967–975.
[61] Sinclair, H.D., Sayer, Z.R., Tucker, M.E (1998) Carbonate Sedimentation during early foreland basin subsidence: the Eocene succession of French Alps. in:V. P. Wright, and T.P. Burchette (Eds.), Carbonate Ramps: Geological Society, London, Special Publications., no.149, p.205–228.
[62] Taghavi, A,A., Mørk, A., Emadi, M,A (2006) Sequencestratigraphically controlled dingenesis governs reservoir quality in the Carbonate Dehluran Field. Southwest Iran. Petroleum Geoscience. Vol. 12, pp, 115–126.
[63] Tucker, M.E., Bathurst, R.G.C (1990) CarbonateDiagenesis. Reprint Series Volume 1 of the International Association of Sedimentologists. v 312 pp.
[64] Tucker, M.E (1993) Carbonate Diagenesis and sequence stratigraphy. In: Wright, V.P., (Ed), Sedimentary review/1, Blackwell. Scientific Publication, p. 51–72.
[65] Tucker, M.E (1991) Sedimentary petrography, Black scientific pub., 260p
[66] Tucker, M.E (2001) Sedimentology Petrology: an introduction to the origin of sedimentary rocks: Blackwell, Scientific Publication, London, 260 p.
[67] Tucker, M.E., Wright, V.P (1990) Carbonate Sedimentology: Black well, London, 482 p.
[68] Warren, J.K (1989) Evaporate Sedimentology: Importance in Hydrocarbon Accumulation, Prentice Hall, Englewood Gliffs, 285p.
[69] Warren, J.k (2000) Dolomite: occurrences, evolution and economical important association, Earth science Review, v. 52, 1–87.
[70] Warren, J.K (2006) Evaporites: Sediments, Resources and Hydrocarbons. Springer Verlag, Brunei, 1035 p.
[71] Whittle, G.L., Alshahran, A.S (1994) Dolomitization and certification of Early Eocene Rus Formation in Abu Dhabi, United Arab Emirates, Sedimentary Geology, v. 92, p. 273–258.
[72] Wilson, J.L (1975) Carbonate facies in geological history. Springer, Berlin–Heidelberg, New York. p. 471.
[73] Wilson M.E.J., Evans M.J., Oxtoby N.H., Nas D.S (2007) Donnelly T. & Thirlwall M., Reservoir quality, textural evolution and origin of fault-associated dolomites, AAPG Bulletin., v. 91, PP. 1247-1273.
[74] Witt, W., Gokdag, H (1994) Orbitolinid Biostratigraphy of rhe Shuaiba formation (Aptian), Oman Implication for Reservoir Development. In Micropalaeontology and Hydrocarbon Exploration in the Middle East. Edited by M.D. Simmons. Chapman & Hall, London, 418 pp.
[75] Wynd, j.c (1965) Biofacies of the Iranian Oil Consortium Agreement Area, IOOC. Rep. no. 10.
)