تعیین درجه پختگی مواد آلی سازند سرچاهان با استفاده از انعکاس گراپتولیت

نوع مقاله : مقاله پژوهشی

چکیده

به منظور تعیین درجه پختگی (بلوغ) مواد آلی سازند سرچاهان در منطقه تنگ زاکین در شمال بندرعباس، نمونه‌های سطح‌الارضی انتخاب و مورد ارزیابی "راک اِول" و با تهیه قرص مقطع ضخیم، مورد مطالعه میکروسکوپی قرار گرفتند. نمونه‌ها غالباً حاوی گراپتولیت بودند که با بررسی میکروسکوپی و شناسایی گراپتولیت‌ها انعکاس آنها اندازه‌گیری شد. همچنین اسلایدهای تهیه شده از کروژن در نور گذرا مورد بررسی قرار گرفتند. از کروژن استخراج شده نیز تجزیه عنصری به عمل آمد. انعکاس گراپتولیت، رنگ کروژن، فلورسانس‌زایی مواد آلی لیپتینیتی و نتیجه آنالیز عنصری کروژن، همگی نشان دهنده پختگی مواد آلی رسوبات سازند مذکور در منطقه تنگ زاکین در مراحل پایانی نفت‌زایی و اوایل گاززایی می‌باشند
 

کلیدواژه‌ها


عنوان مقاله [English]

Thermal Maturity Determination of Sarchahan Formation (NE Bandar Abbas, South Iran) Using Graptolite Reflectance (GRo%)

چکیده [English]

In order to determine the maturity of the organic matter of Sarchahan Formation in northern Bandar Abbas, 15 outcrop samples were collected from Tang-e-Zakin, North Syahoo village, 70 km. from the city of Bandar Abbas. The Reflectance of Graptolites (%GRo) were measured by a reflected light microscope (MPV-SP) and histograms were plotted. The Mean Random Reflectance of these samples were 1.11% which indicate the catagenetic stage of maturity. These samples were also subjected to Rock- Eval Pyrolysis. The average Tmax for these samples is 455
C that indicates the end of oil generation window and early stage of gas generation. The Gahkum Formation (Silurian shales) as a whole was reported as overmature and its organic matter considered to have graphitic stage of maturity. Nevertheless Gahkum Fm. was divided into Syahoo Fm. (Ordovician) and Sarchahan Fm. (lower Silurian) on the basis of their biozones. On the other hand, this study geochemically investigated Sarchahan Formation separately with the help of Rock-Eval data, TAI, elemental analysis of kerogen and measurements of graptolite reflectance (Gro%), and concluded that it is in the catagenetic stage of maturity and emphasis on the Silurian strata for future hydrocarbon exploration in Iran.

کلیدواژه‌ها [English]

  • Gahkum Formatiom
  • Sarchahan Formation
  • Graptolite Reflectance
  • GRo%
  • Elemental Analysis
[1] Rahman M. & Kinghorn R.R.F., “A practical classification of Kerogen related to hydrocarbon generation”, Journal of  Petroleum Geology, Vol. 18, Issue. 1, 18 December, 2007.
[2] Taylor G.H., Teichmuller M., Davis A.C., Diessel E.K., Lttke R. & Rbert P., Organic petrology, Gebruder Borntraeger, Berlin, 1998.
[3] Moujahed I. Husseini M., “Tectonic and depositional model of the Arabian and adjoining plates during the Silurian-Devonian”, AAPG, Vol. 75, No. 1, pp. 108-120, 1991.
[4] Mahmoud D., “The lower silurian qaliba formation of Saudi Arabia”, Geo Arabia, Vol. 5, No. 1, 2000.
[5] Afifi A., “Paleozoic stratigraphy and hydrocarbon habitat of the Arabian plate”, Geo Arabia, Vol. 6, No. 3  pp. 407-441, 2001.
[6] Schenk Ch.J. & Pollastro R.M., “Assessment of undiscovered oil and gas resources in the Qusaiba-Paleozoic petroleum system of the greater Rub ‘al Khali Basin, Arabian Peninsula”, Geo  Arabia, Vol. 5, No. 1, 2000.
[7] Ghavidel Syuki M. & Khosravi M.E., “Investigation of lower paleozoic sediments at Tang-e-Zakeen of Kuh-e-Faraghan and introduction of the Seyahou and Sarchahan formations in the Zagros basin Geo sience”, Geological Survey of Iran. (GSI), Vol. 4, No. 14, 1995.
[8] Alsharhan A.S. & Nairn A.E.M., Sedimentary basins and petroleum geology of the Middle East, Amsterdam, The Netherlands, Elsevier Science B.V., 942 p. 1997.     
[9] Bordenave M.L., Fozoonmaye M.C. & Nilly A.R., Geochemical Report of Fars Province, NIOC., 1181, 1971.
[10] Pollastro R.M., “Total petroleum systems of the paleozoic and jurassic in greater Ghawar and adjacent provinces of Saudi Arabia”, US Geological Survey Bulletin, 2202,1-100, 2003.
[11] Tavallaee M., Eftekhari N., Kassaee M. & Moeenpour M., Type and maturity of organic matters in Silurian sediments of N-Bandar Abbas, RIPI Project No. 41210160, 1379.
[12] Ruppert E.E. & Barners R.D., Invertebrate  Zoology, 6th Ed., College Publishing Forth Worth, 1994.
[13] Cole G.A., Graptolite, Chitinozoan reflectance and its relationship to geochemical maturity indicators in Silurian Qusaiba Shale, Energy Citation Database, pp. 1443-145, USA, May 13, 2001.
[14] Bertrand R., “Correlation among the reflectance of vitrinite, graptolite and scholecodonts”, Organic Geochemistry, Vol. 15, No. 6, pp. 574-565, 1988.
[15] Goodarzi F., Buchardt B.J. & Lewan M.D., “Thermal maturity of lower paleozoic sedimentary successions in Arctic Canada”, AAPG Bulletin, Vol. 80, No. 7, pp. 1065-1084, 1996.
[16] Teichmuller M., “Organic petrology of source rocks history and states of the Arts”, Advances in Organic Geochemistry, Vol. 10, pp. 581-599, 1986.