محیط رسوبی و چینه‌نگاری سکانسی سازند داریان در میدان گازی پارس جنوبی

1-             آقانباتی، ع. ، ١٣٨٣،  زمین­شناسی ایران، سازمان زمین­شناسی و اکتشافات معدنی، ٥٨٦ ص.

2-            صفری، ف.، (1386). میکروبیواستراتیگرافی سازند داریان در برشهای سیوند و دشتک در ناحیه فارس و تطابق آن با چاه سروستان -3. پایان نامه کارشناسی ارشد دانشگاه تهران، 165 صفحه.

3-                  Aigner, T., M., Schauer, W-D. Junghans,  and L., Reinhardt 1995, Outcrop gamma-ray logging and its applications: examples from the German Triassic: Sedimentary Geology,v. 100, p. 47-61.

4-                  Al-Ghamdi, N. M , 2006, Facies, Sequence Framework, and Evolution of RudistBuildups, Shuaiba Formation, Saudi Arabia: MSc thesis, Blacksburg, Virginia, May 19, 2006.

5-                  Alsharhan , A. S. and A. E, Nairn 1997, Carbonate Pltform Model of Arabian Cretaceous Reservoirs in Sedimentary basins and petroleum of the Middle East: Elsevier, chapter 15.

6-                  Alsharhan, A.S., and A.E.M., Nairn 1986,  A review of the Cretaceous formations in the Arabian Peninsula and Gulg: Part 1.Lower Cretaceous (Thamama Group) stratigraphy and paleogeography: J. Pet.Geol., v.9; p. 365-92.

7-                  Banner, F. T. and M. D., Simmons 1994, Calcareous algae and foraminifera as water-depth indicators: an example from the Early Cretaceous carbonates of northeast Arabia, In: Micropalaeontology and Hydrocarbon Exploration in the Middle East (Ed. M.D. Simmons), pp. 243–252, British Micropalaeontol. Soc. Publ. Series. Chapman & Hall, London.

8-                  Banner, F.T., E. M., Finch M. D., Simmons 1990, On Lithocodium Elliott (calcareous algae); its paleobiological and stratigraphical significance,J. Micropaleont. v.9, p. 21–36.

9-                  Bernaus: J. M., A. A., Vanneau, and E., Caus 2003, Carbonate platform sequencestratigraphy in a rapidly subsiding area: the Late Barremian–Early Aptian of the Organya basin: Spanish Pyrenees Sedimentary Geology, v. 159, p. 177–201.

10-              Bosellini, A., 1999, Stratigraphic evidence for an Early Aptian sea-level fluctuation: the  Graua Limestone of south-eastern Ethiopia: Cretaceous Research, v. 20,  p.783–791.

11-              Burchette, T. P. and V. P., Wright 1992, Carbonate ramp depositional systems: Sedimentary Geology, v.79, p. 3.

12-              Buxton, M. W. N. and Pedley 1989, a standardized model for Tethyan Tertiary carbonate ramps: Journal of the Geological Society, v. 146, p. 746-748.

13-              Catuneanu, O, 2006, Principles of Sequence Stratigraphy: (first Edition) Elsevier, Amsterdam. 375p.

14-              Cherchi, A., and R., Schroeder, 2006, Remarks on the systematic position of Lithocodium Elliott a problematic microorganism from the Mesozoic carbonate platforms of the Tethyan realm: Faciesv.  52, p. 435–440.

15-              Cherechi,  A., and  R.,  Schroder  2004, Evolution  of  orbitolinid  foraminifers  and  anoxic event  A comment  on  an  article  by  J,Guex, Eclogae  geol.helv.  94  (2001). Eclogae  Geol. Helv, v. 97; p. 441 – 444.

16-              Conrad, M. A., and B., Clavel 2008, A Lithocodium and Bacinella signature of a late Hauterivian, local microbial event: the Urgonian limestone in South-East France: Geologia Croatica, v. 61, p. 239–250.

17-              Elliott G. F., 1956, further records of fossil calcareous algae from the Middle East: Micropaleontology, v. 2; p. 327–334.

18-               Embry, A.F., J.E., Klovan 1971, A late Devonian reef tracton northeastern Banks Island: N.W.T. - Bull. CanadianPetrol. Geol., v. 19, p.730-781.

19-               Emery D., and K. J., Myers 1996, Sequence stratigraphy: Oxford, UK7 Blackwell, 297. P.

20-               Flügel, E., 2004, Microfacies of Carbonate Rocks: Analysis, Interpretation and Application: Springer Berlin, Heidelberg, New York, 976 p.

21-               Greselle, B., B., Pittet 2005, Fringing carbonate platform at the Arabian Plate marginin northern Oman during the Late Aptian-Middle Albian: Evidence for highamplitudesea-level changes: Sedimentary Geology, v. 175, p. 367-390.

22-               Heydari, E., 2008, Tectonics versus eustatic control on supersequences of the Zagros Mountains of Iran: Tectonophysics, v. 451,  p. 56–70.

23-               Hosseini, S. A, and M. A., Conrad 2008, Calcareous algae, foraminifera and sequence stratigraphy of the Fahliyan Formation at Kuh-e-Surmeh (Zagros Basin, SW of Iran): Geologia Croatica, p. 215 –237.

24-               Hosseinyar, G. H., H., Rahimpour-Bonab, A., Asadi Esksndar and M., Asgharian Rostami 2009, Survey of the diagenesis process and effect these process on reservoir quality of the Kangan formation in South Pars Field, Nature Precedings.

25-               Hottinger, L., 1982, larger foraminifera, giant cells with a historical background: Naturwissenschaften, v. 69, p. 361.

26-               Hughes, G. W., 2000, Bioecostratigraphy of the Shu’aiba Formation, Shaybah field, Saudi Arabia, GeoArabia,  v. 5, p. 4.

27-               Hunt, D., and M. E., Tucker 1995, Stranded parasequences and theforced regressive wedge systems tract: deposition during baselevelfall – reply: Sedimentary Geology, v. 95, p. 147–160.

28-               parasequences and the forced regressive wedge systems tract: deposition during baselevel fall: Sedimentary Geology, v. 81, p. 1–9.

29-              Husinec, A.,  I., Velic´, L., Fucek, I., Vlahovic, D., Maticec, O., stric and T., Korbar 2000, Mid Cretaceous orbitolinid (Foraminiferida) record from the islands of Cres and Losinj Croatia) and its regional stratigraphic:  Cretaceous Research correlation, v. 21, p. 155–171.

30-              Husinec, A., and B., Sokac 2006, Early Cretaceous benthic associations (foraminifera and calcareous algae) of a shallow tropical-water platform environment (Mljet Island, southern Croatia): Cretaceous Research, v. 27, p. 418-441.

31-               Immenhauser, A., W., Schlager, S. J., Burns,  R. W. , Scott, T., Geel, J. , Lehmann, S., Van der Gaast, and L. J. A., Bolder Schrijwer 1999, Late Aptian to Late Albian sea-level fluctuations constrained by geochemical and biological evidence (Nahr Umr Formation, Oman): J. Sed. Res, v. 69, p. 434–466.

32-               Kastner, M., I., Schulke, J., Winsemann 2008, Facies architecture of a Late Jurassic carbonate ramp: the Korallenoolith of the Lower Saxony Basin: Int J Earth Sci (Geol Rundsch), v. 97, p. 991–1011.

33-               Krobicki, M.,  and  B., Olszewska 2005, Urgonian-type microfossils in exotic pebbles of the Late Cretaceous and Palaeogene gravelstones from the Sromowce and Jarmuta formations (Pieniny Klippen Belt, Polish Carpathians): Studia Geologica Polonica, v. 124, p.  215–235.

34-               Loeblich, A.R., and H., Tappan 1987, Foraminiferal genera and their classification,: 2 Vol., 1182 p., Van Nostrand Reinhold Co, New York.

35-               Lucia, G. F., 1990, Carbonate Reservoir Characterization: ISBN, v. 964, p. 4865.

36-               Mancinelli, A., M., Chiocchini,  and B., Coccia  2003, Orbitolinidae and Alveolinidae (Foraminiferida) fromthe uppermost Albian-lower Cenomanian of Monti d’Ocre (Abruzzi, Italy): Cretaceous Research, v. 24, p. 729–741.

37-              Matsumaru, K ., 2005, Praeorbitolinoides, a new Orbitolinid foraminiferal genus from the  Lower Aptian (Cretaceous) of Hokkaido, Japan. Micropaleontology, v. 51, p. 93-99.

38-              Michelsen, O., and M., Danielsen 1996, Sequence and systems tract interpretation of the epicontinental Oligocene deposits in the Danish North Sea: Geological Society, London,Special Publications 1996, v. 117, p. 1-13.

39-              Mitchum, R. M., 1977, Glossary of terms used in seismic stratigraphy, In: Payton, C. Z (ed.): nSeismic stratigraphy_applications to hydrocarbon exploration, Amer. Ass. PetrolGeol. Bull, v. 26, p.  205-212.

40-              Murris, R. J., 1980, The Middle East: stratigraphic evolution and oil habitat: American Association of Petroleum Geologists Bulletin, v. 64, p. 597–618.

41-              Moullade, M., B., Peybernes, J., Rey and  P., Saint-Marc 1985, Biostratigraphic interest and paleobiogeographic distribution of early and mid-Cretaceous Mesogean orbitolinids (Foraminiferida): Journal of Foraminiferal Research, v. 15, p. 149–158.

42-               Olivier, N., B., Pittet, W., Werner, P., Hantzpergue, C., Gaillard 2008, Facies distribution and coral-microbialite reef development on a low -energy carbonate ramp (Chay Peninsula, Kimmeridgian and western France: Sedimentary Geology, v. 205, p. 14–33

43-               Pittet. B., S., Frans, P., Van Buchem, H., Hillgartner,  P., Razin,  J., Grotsgh,  H., Drostes  2002, Ecological succession, palaeoenvironmental change, Ecological succession, palaeoenvironmental change of Barremian – Aptian  shallow-water carbonates in northern Oman: Sedimentology, v. 49, p. 555–581.

44-               Posamentier, H. W.,  M. T., Jervey, and P. R., Vail 1988, Eustatic controls on clastic deposition, I. Conceptual framework. In: Wigus, C.K. (Editor). Sea-Level Change: An Integrated Approach; Society of Economic Paleontologists and Mineralogists Special Publication, v. 42, p. 110-124.

45-               Reiss, Z., and L., Hottinger 1984, the Gulf of Aqaba. Ecological Micropaleontology: Springer, Berlin, 283.

46-               Schroeder R., 1964, Orbitoliniden-biostratigraphie des Urgon  nordostlich  von Ternel (Spanien). Neues  Jahrbuch  fur  Geologie  und  Palaontologie,  Monatshefte,  p. 462- 474.

47-               Schroeder, R., 1975,  General  evolutionary trends  Orbitolinas . Rev. Espanola micropal .Numero  Especial, p. 117-123.

48-               Selly, R., 1939, Ancient Sedimentaray Environments: ISBN. 964-03-4488-5.

49-               Sampo, M., 1969, Microfacies and Microfossils of the Zagros area. Southwestern Iran (from Pre-Permian-Miocen).E.J. Brill, Leiden, 102 p.

50-               Scott, R., W., 1990a, Chronostratigraphy of the Cretaceous carbonate shelf, southeastern Arabia. In: A.H.F, Robertson, M.P. Searle and A.C. Ries (Eds.), The Geology and Tectonics of the Oman Region: Geol.Soc.Sep.Publ., v. 49, p. 89-108.

51-               Shakib, S.S., 1994, Palaeoenvirenmental and biostrathigraphic significance of foraminiferal associations from the early Cretaceous sediments of southwest Iran. Micropalaeontology and Hydrocarbon Exploration in the Middle East, p. 129-149.

52-               Simmons, M.D., and M.B., Hart, 1987,  The biostratigraphy and microfacies of the Early to mid-Cretaceous carbonate of Wadia Miaidin, Central Oman Mountain.In M. B. Hart(Ed.) Micropalaeontology of Carbonate Environment, Harwood. Chichester, 176-207.

53-               Simmons. M. D., 1994, Micropalaeontological biozonation of the Kahmah Group (Early Cretaceous), Centeral Oman Mountains. In: Micropalaeontology  and Hydrocarbon Exploration in the Middle East (Ed. M.D. Simmons), pp. 243–252,  British Micropalaeontol. Soc. Publ. Series. Chapman & Hall, London.

54-              Taylor, S. P., Sellwood, B. W., 2002, the context of lowstand events in the Kimmeridgian (Late Jurassic) sequence stratigraphic evolution of the Wessex–Weald Basin, Southern England: Sedimentary Geology, v. 151, p. 89–106.

55-              Tucker, M.E., and F., Calvet, D., Hunt, 1993, Sequence Stratigraphy of carbonate ramps: system tracts, models and application to Muschelkalk carbonate platform of eastern Spain, In: Posamentier, H.W, Summerhayes, C.P, Haq, B.U and Allen, G.P (Eds.): Sequence Stratigraphy and facies associations: Spec.Publ.Int.Ass Sedimentol, v. 18, p. 397-415.

56-               Tucker, M. E., and V. P., Wright, 1990, Carbonate sedimentology: Blackwell Scientific Publications, 482 p.

57-               Van Wagoner, J. C., R. M. Jr., Mitchum, H. W., Posamentier, and P. R., Vail 1988, Seismic stratigraphy interpretation using sequence stratigraphy:  part 2: key definitions of sequence stratigraphy, in: Atlas of Seismic Stratigraphy (A.W. Bally, Editor): American Association of Petrologists and Geologists Student Geology, v. 27, p. 11-14.

58-              Velic, I., 2007,  Stratigraphy and Palaeobiogeography of Mesozoic Benthic Foraminifera of the Karst Dinarides (SE Europe).

59-              Velic, I., 1988, Lower Cretaceous benthic foraminiferal biostratig raphy of the shallow water carbonates of the Dinarides: Revue de  Pale´obiologie, Volume Spe´cial 2 (Benthos ’86), p.  467– 475.

60-               Velic, I., and  I., Vlahovic´ 1994, Foraminiferal assemblages in the  Cenomanian of the Buzet-  Savudrija area (northwestern Istria, Croatia): Geologia Croatica , v. 47, p. 25–43.

61-               Vilas, L., J. P., Masse, and C., Arias 1995, Orbitolina episodes in carbonate platform evolution the early Aptian model from SE Spain: Palaeogeography, Palaeoclimatology Palaeoecology, v. 119, p. 35–45.

62-              Witt. W., and H., Gokdag 1994, Orbitolinid biostratigraphy of the Shuaiba Formation (Aptian), Oman implication for reservoir development. In: Micropalaeontology  and Hydrocarbon Exploration in the Middle East (Ed. M.D. Simmons), pp. 243–252,  British Micropalaeontol. Soc. Publ. Series. Chapman & Hall, London

63-               J. E., Whittaker, R. W., Jones, and F.T., Banner 1998, Key Mesozoic Bentic Forminifera of the middle east. Natural history Museum.