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  • Neocomian Fahliyan formation carbonates in the oil well X2 (Dorood oil field, Persian Gulf): Biostratigraphic data from benthic foraminifera and algae

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کد مقاله : IJES-1712-1152 (R2) بازدید : 162 صفحه: 173 - 182

10.30495/ijes.2019.667376

نوع مقاله: پژوهشی

Neocomian Fahliyan formation carbonates in the oil well X2 (Dorood oil field, Persian Gulf): Biostratigraphic data from benthic foraminifera and algae

محورهای موضوعی : Mineralogy

لیلا رستمی 1 , سیدحمید وزیری 2 , داود جهانی 3 , علی سلگی 4 , مرتضی طاهرپور خلیل آباد 5 , ایوانا زورن گراویک 6 , احمد یحیایی 7

1 - گروه زمین شناسی، دانشگاه آزاد اسلامی واحد علوم و تحقیقات
2 - گروه زمین شناسی دانشگاه آزاد اسلامی واحد تهران شمال
3 - گروه زمین شناسی، دانشگاه آزاد اسلامی واحد تهران شمال
4 - گروه زمین شناسی، دانشکده علوم پایه، دانشگاه آزاد اسلامی واحد علوم و تحقیقات
5 - باشگاه نخبگان و محققان جوان، دانشگاه آزاد اسلامی واحد مشهد، مشهد، ایران
6 - دانشکده جغرافیا، دانشگاه بلگراد
7 - شرکت نفت فلات قاره ایران

تاریخ دریافت : 1396/10/21 تاریخ پذیرش : 1397/09/13 تاریخ انتشار : 1398/04/10

کلید واژه: Persian Gulf, Fahliyan Formation, algae, benthic foraminifera, Berriasian-Hauterivian,

چکیده مقاله :

The Fahliyan Formation of the Khami Group is the most important oil and gas reservoir in southwestern Iran. The formation attains a thickness of 435.5 m in the oil well X2 in Dorood oil field, Persian Gulf. It is represented mainly by thin-bedded limestones. This formation unconformably overlies the evaporate late Jurassic Hith Formation and conformably underlies the Gadvan Formation. Integrated palaeontological and sedimentological studies supported by an analysis of 150 thin-sections led to the identification of 21 benthic foraminiferal genera dominated by agglutinated forms with an additional 8 algal genera. Two foraminiferal biozones of Berriasian through Hauterivian age include the Pseudochrysalidina (Dokhania) arabica acme zone and Pseudocyclammina lituus- Coscinoconus assemblage zone, and an algal zone includes the Salpingoporella annulata range zone have been recognized. The correlation of the lower Cretaceous petroleum source rock in the Persian Gulf with regions from Tethyan Realm is limited by the lack of the analog formation that can be used for comparison. In this way, the foraminiferal zones are correlated with coeval zones in south and southwest of Iran.

چکیده انگلیسی:

منابع و مأخذ:


  1. Abedpour M, Afghah M, Ahmadi V and Dehghanian M (2016) Biostratigraphic    and Lithostratigraphic Study of Fahliyan Formation in Kuh-E-Siah (Arsenjan Area, North-East of Fars Province). Open Journal of Geology 6:1605-1618.
    2.
  2. Abyat A, Baghbani D, Afghah M, Kohansal Ghadimvand N and 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.
    3.
  3. Abyat A, Baghbani D, Afghah M and Kohansal Ghadimvand N (2014) Microfacies, depositional environment and sequence stratigraphy of the Fahliyan and Gadvan Formations, Kuh-e-Surmeh section (Zagros Basin, Southwest Iran). Himalayan Geology 35(1): 82-88.
    4.
  4. Adabi MH, Salehi MA and Ghabeishavi A (2010) Depositional environment, sequence stratigraphy and geochemistry of Lower Cretaceous carbonates (Fahliyan Formation), south-west Iran. Journal of Asian Earth Science 39: 148-160.
    5.
  5. Afghah M (2006) Microbiostratigraphy of Fahliyan Formation in Kuhe-e-Gadavan and Ab Siah,  Journal of Sciences 61: 89-107.
    6.
  6. Bahroudi A and Talbot CJ (2003) The configuration of the basement beneath the Zagros Basin. JPG 26: 257-282.
    7.
  7. Banner FT, Finch EM and Simmons MD (1990) On Lithocodiurn Elliott (Calcareous algae); its paleobiological and stratigraphical significance. Journal of Micropalaeontology 9 (1): 21-36
    8.
  8. Bou Dagher-Fadel MK (2008) Evolution and Geological Significance of Larger Benthic Foraminifera. Elsevier, Amsterdam.
    9.
  9. Bruni R, Bucur II and Preat A (2007) Uppermost Jurassic-Lower Cretaceous carbonate deposits from Fara San Martino (Maiella, Italy): biostratigraphic remarks. Studia UBB, Geologia 52(2): 45-54.
    10.
  10. Bucur I (1995) Algues calcaires dans les dépôts du Jurassique supérieur-Crétacé inférieur des Monts Pădurea Craiului. Studii şi Cercetări, Muzeul Bistriţa Năsăud 1: 79-89.
    11.
  11. Bucur I, Săsăran L, Săsăran E and Schuller V (2004) Micropaleontological study of the limestone olistoliths within the Upper Cretaceous wildflysh from Hăşdate (eastern border of the Gilău Mountains). Acta Palaeontol Rom 4: 55-67.
    12.
  12. Bucur I and Săsăran E (2005) Relationship between algae and environment: An Early Cretaceous case study, Trascău Mountains, Romania. Facies 51(1-4): 275-287.
    13.
  13. Carević I, Taherpour Khalil Abad M, Ljubović-Obradović D, Vaziri SH, Mirković M, Aryaei AA, Stejić P and Ashouri AR (2013) Comparisons between the Urgonian platform carbonates from eastern Serbia (Carpatho-Balkanides) and northeast Iran (Kopet-Dagh Basin): Depositional facies, microfacies, biostratigraphy, palaeoenvironments and palaeoecology, Cretaceous Research 40: 110-130.
    14.
  14. Chehrazi A, Rezaee MR and Rahimpour H (2011) Pore-facies as a tool for incorporation of small scale dynamic information in integrated reservoir studies. Journal of Geophys Engineering 8: 202-224.
    15.
  15. Conrad M (1977) The Lower Cretaceous Calcareous Algae in the Area Surrounding Geneva (Switzerland): Biostratigraphy and Depositional Environments. In: E. Flügel (Ed.), Fossil algae, Springer, Heidelberg: 295-300.
    16.
  16. Deini I and Radoičić R (1999) Clypeina dragastani sp. nov., Salpingoporella granieri sp. nov. and other Dasycladalean algae from the Berriasian of eastern Sardinia. Acta Palaeontol Rom 2: 105-123.
    17.
  17. Dragastan O, Popescu IS and Popescu I (2005) Cretaceous microfacies and algae from the central eastern sectors of the Moesian carbonate platform. Acta Palaeontol Rom 5: 141-162.
    18.
  18. Feghhi A (2010) Study of Microfacies and Sequence Stratigraphy of Fahliyan Formation in Marun Oil Field, Southwest Iran. Master Thesis, Science at the University of Petroleum University of Technology Exploration and Production Department Tehran, Tehran 83 p.
    19.
  19. Gollesstaneh A (1965) Micropalaeontological study of the Upper Jurassic and Lower Cretaceous of Southern Iran. Unpublished Ph.D. Thesis, University College London 629 p.
    20.
  20. Hassani-Giv M, Soleimani B and Ghalavand H (2016) Lithofacies variation of Lower Cretaceous sedimentary succession: An interaction of paleo-high and mixed carbonate-clastic system and its consequence on the distribution of reservoir units in Abadan plain, SW-Iran. Journal of Biodiversity and Environmental Sciences 10(4):187-200.
    21.
  21. Hosseini A and Conrad M (2008) Calcareous algae, foraminifera and sequence stratigraphy of the Fahliyan Formation at Kuh-e-Surmeh, Geologia Croatica 61(2-3): 215-237.
    22.
  22. Husinec A and Sokač B (2006) Early Cretaceous benthic associations (foraminifera and calcareous algae) of a shallow tropical-water platform environment (Mljet Island, southern Croatia). Cretaceous Research 27: 418-441.
    23.
  23. Ivanova D and Kolodziej B (2004) New foraminiferal data on the age of Stramberk-type limestones, Polish Carpathians. CR ACAD BULG SCI 57(12): 12-69.
    24.
  24. Ivanova D and Kolodziej B (2010) Late Jurassic-Early Cretaceous Foraminifera from Štramberk-Type Limestones, Polish Outer Carpathians. Studia UBB Geologia 55(2): 3-31.
    25.
  25. Jaffrezo M and Renard M (1979) Eléments en traces de calcaires à Dasycladales et Charophytes. Bull. Cent. Rech. Explor. Prod. Elf Aquitaine 3: 639-649.
    26.
  26. Jamalian M, Adabi MH, Moussavi MR, Sadeghi A, Baghbani D and Yriyafar B (2010) Facies characteristic and paleoenvironmental reconstruction of the Fahliyan Formation, Lower Cretaceous, in the Kuh-e Siah area, Zagros Basin, southern Iran. Facies 57: 101-122.
    27.
  27. Jamalian M, Adabi MH, Moussavi MR, Sadeghi A, Baghbani D and 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.
    28.
  28. James GA and Wynd JG (1965). Stratigraphical nomenclature of Iranian Oil Consortium agreement area: American Association of Petroleum Geologists 49: 2182-2245.
    29.
  29. Kalantari A (1975) Microbiostratigraphy of the Sarvestan Area, Southwestern Iran. National Iranian Oil Company, Geological Laboratories publication 5(7): 26 p.
    30.
  30. Kaminski MA (2004) The Year 2000 Classification of the Agglutinated Foraminifera. In: Bubík M, Kaminski MA (Eds.), Proceedings of the Sixth International Workshop on Agglutinated Foraminifera. Grzybowski Foundation, Special Publication: 237-255.
    31.
  31. Kheradpir A (1975) Stratigraphy of the Khami group in Southwest Iran. O.S.C.I. Report No. 1235.
    32.
  32. Khosravi M, Lasemi Y and Feizi M (2009) Platform to basin facies transition in the Lower Cretaceous Fahliyan Formation: evidence for the formation of garu intra. Proceedings of the 1st International Petroleum Conference and Exhibition. European Association of Geoscientists and Engineers, EAGE, Shiraz, Iran.
    33.
  33. Kobayashi F and Vuks VJ (2006) Tithonian–Berriasian foraminiferal faunas from the Torinosu-type calcareous blocks of the southern Kanto Mountains, Japan: their implications for post-accretionary tectonics of Jurassic to Cretaceous terranes. Geobios 39(6): 833-843.
    34.
  34. Krajewski M and Olszewska B (2007) Foraminifera from the Late Jurassic and Early Cretaceous carbonate platform facies of the southern part of the Crimea Mountains, Southern Ukraine. Annales Societatis Geologorum Poloniae 77: 291-311.
    35.
  35. Lasemi Y and Feyzi M (2007) Platform and Off-Platform Facies of Fahliyan Formation: Evidence for Intrashelfbasin in Southwest of Iran. 25th Symposium of Geology, Geological Survey of Iran: 84-85 (in Persian).
    36.
  36. Loeblich AR and Tappan H (1987) Foraminiferal Genera and their Classification, Van Nostrand Reinhold New York 970 p, 847 pls.
    37.
  37. Masters CD, Klemme HD and Courry AB (1982) Assessment of Undiscovered Conventionally Recoverable Petroleum Resources of the Arabian-Iranian Basin. Geological Survey Circular 881: 1-12.
    38.
  38. Moallemi SA (2000) Microfacies, Sedimentary Environment and Variation of Porosity of Fahliyan Formation in Khark Area. Master Thesis, Science at the University of Azad, Tehran, Iran 107 p. (in Persian).
    39.
  39. Mohammad-Khani H (2003) Sedimentary Environment Reconstruction and Sequence Stratigraphy of Fahliyan Formation at Khaviz and Rag-sefid Oil Field, South Dezful Embayment. Master Thesis, Science at the University of Tarbiyat-Moalem, Tehran, Iran, 68p. (in Persian).
    40.
  40. Mosadegh H and Shirazi M (2009) Algal biozonation of Fahliyan Formation (Neocomian) in the Zagros Basin, Iran. European Geoscience Union, Geophysical Research Abstracts EGU 2009-8507, 11.
    41.
  41. Parvaneh Nejad Shirazi M (2008) Calcareous Algae from the Cretaceous of Zagros Mountains (SW Iran). World Applied Sciences Journal 4(6):803-807.
    42.
  42. Rastegar Lari AL (2009) Paleoenvironment and Sequence Stratigraphy of Fahliyan Formation in central Fars, Journal of Applied Geology 2: 111-120.
    43.
  43. Renaud L and Gildas R (2000) Iran-Dorood Filed reservoir study, part1: Sedimentary model and correlations. Iranian Offshore Oil Company (IOOC) 209 p.
    44.
  44. Rollinston HR, Searle MP, Abbasi IA, Al-Lazki A and Al-Kindi, M.H. (2014) Tectonic evolution of the Oman Mountains. Geological Society, Special Publication 392, London 471 p.
    45.
  45. Rostami L, Vaziri SH, Jahani D, Solgi A, Taherpour Khalil Abad M and Yahyaei A (2017) Lithostratigraphy and biostratigraphy of the Fahliyan Formation in oil well no. D-101 P, Dorood oil field, Persian Gulf. 35th National Geosciences Conference, Geological Survey of Iran.
    46.
  46. Sahraeyan M, Bahrami M, Hooshmand M and Ghazi S (2013) Sedimentary facies and diagenetic features of the Early Cretaceous Fahliyan Formation in the Zagros Fold-Thrust Belt, Iran. Journal of African Earth Sciences 87: 59-70.
    47.
  47. Shakib SS (1994) Paleoenvironmental and biostratigraphic significance of foraminiferal associations from the Early Cretaceous sediments of southwest Iran, In: Simmons, M.D. (Ed.), Micropalaeontology and Hydrocarbon Exploration in the Middle East. British Micropalaeontological Society Publication Series, Chapman & Hall, London: 127-157.
    48.
  48. Soleimani B, Hassani-Giv M and Abdollahi Fard I (2017) Formation Pore Pressure Variation of the Neocomian Sedimentary Succession (the Fahliyan Formation) in the Abadan Plain Basin, SW of Iran. Geofluids Article ID 6265341, 13 p.
    49.
  49. Wynd JG (1965) Biofacies of the Iranian Oil Consortium Agreement Area: Iranian Oil Operating Companies. Geological and Exploration Division Report 1082, 89 p.
    50.
  50. Yilmaz IO (1999) Taxonomic and Palaeogeographic Approaches to the Dasyclad Algae in the Upper Jurassic (Kimmeridgian)-Upper Cretaceous (Cenomanian) Peritidal Carbonates of the Fele (Yassibel) Area (Western Taurides, Turkey), Turkish Journal of Earth Science 8: 81-101.
    51.
  51. Ziegler MA (2001) Late Permian to Holocene paleofacies evolution of the Arabian plate and its hydrocarbon occurrences, GeoArabia 6: 445-504.
    52.

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