Studying Maturity and Migration Routes Using Two-Dimensional Modeling in a number of Dezful Dam Oilfields
Subject Areas : Petroleum GeologyAshkan Maleki 1 , Seyed Ali Moallemi 2 , Mohammad Hossein Saberi 3 , Mohammad Hassan Jazayeri 4
1 -
2 -
3 -
4 -
Keywords: One-dimensional modeling Two-dimensional modeling Dezful embayment Migration model,
Abstract :
To the southwest of Iran there are large reservoirs of oil and gas including Jurassic and Cretaceous carbonates, with good source rocks in the succession of the Early Cretaceous and Jurassic. The purpose of this study was to investigate the production, migration and characterization of Pabdeh, Kazhdumi, Garru and Serglu source rocks in the study area. For this purpose, burial history and one-dimensional thermal modeling in four wells and two-dimensional modeling in one section for the study area were evaluated using Openuploo software to determine the maturity of layers and hydrocarbon outflow. Comparison of measured vitrinite temperature and reflectance values with model results was used for model calibration. The results of one-dimensional modelling of the burial and thermal history in this study show that the Sergloo, Grove and Kazhdumi formations have reached maturity and have had hydrocarbon outflow, but the Pabdeh Formation has not reached sufficient maturity for hydrocarbon maturation and production. The results of migration model in the studied section show that the two Early Cretaceous and Middle Cretaceous hydrocarbon systems were separated by Kazhdumi Formation and therefore hydrocarbon migration in deeper layers of Kazhdumi was mostly lateral to Abadan plain. The hydrocarbon produced from the Kazhdumi Formation, in addition to ornithologically rearing the upper layers, migrated to the Ilam and Sarvak layers due to the general slope of the layers laterally and toward the Abadan plain. In general, the process of maturation of source rocks decreased from east to west of the study area.
[1]اشکان ح. ر، (1387) "ژئوشیمی آلی و کاربرهای آن در اکتشاف نفت" انتشارات مناطق نفت¬خیز جنوب، 380صفحه.
[2] آقانباتی، ع. (1383) "زمین¬شناسی ایران" انتشارات سازمان زمین¬شناسی و اکتشاف معدنی کشور، تهران، ص 586.
[3] اورک ز.، کردی م.، کریمی ا. ر.، "ارزیابی ژئوشیمیایی و گسترش رخسارههای آلی سازند پابده در سواحل شمالغربی خلیج فارس و جنوب فروافتادگی دزفول با استفاده از تجزیه و تحلیل راک- اول"، پژوهش های چینه نگاری و رسوب شناسی، دوره 34، شماره 3، صفحات 95-108، 1397.
[4] درویش¬زاده ع، زمین¬شناسی ایران، انتشارات امیرکبیر، 1394.#3 [5] سراج، م. (1384) " تحلیل ساختاری مقدماتی میادین نفتی مناطق نفت خیز جنوب (محدوده فروافتادگی دزفول شمالی)، گزارش پ-5613، اهواز.
[6] صابری، م. ح.، اشرفی، ط.، خالقی، م. (1396) "مدل سازی یک بعدی حوضهی رسوبی در میدان گازی تابناک، منطقه ی فارس ساحلی، ایران"، زمین شناسی کاربردی پیشرفته، 7(3)، 65-75.
[7] مطیعی، ه. 1374. زمین شناسی ایران: زمین شناسی نفت زاگرس 2-1. سازمان زمین شناسی کشور.
[8] معماریانی م، بنی اسد، ع. (1390) "مطالعه بیومارکری نفت مخزن آسماری، میادین واقع در حاشیه شمال شرق دزفول فروافتاده" مجله زمین شناسی نفت ایران، جلد 1، شماره 1.
[9] ALA, M.A., KINGHORN, R.R.F., & RAHMAN, M.T., 1980, Organic geochemistry and source rock characteristics of the Zagros petroleum province, southwest Iran. Journal of Petroleum Geology, 3(1), 61-89.
[10] ALAVI, M., 2007. Structures of the Zagros fold-thrust belt in Iran. American Journal of science, 307(9), 1064-1095.
[11] BANIASAD, A., RABBANI, A.R., SACHSE, V. LITTKE, R., MOALLEMI, A., & SOLEIMANY, B., 2016, 2D Basin Modeling Study of the Binak Trough, Northwestern Persian Gulf, Iran. Marine and Petroleum Geology, 77, 882–97.
[12] BAURE, F. LITTKE, R. WIELENS, H. LAMPLE, C., & FUCHS, T., 2010, Basin Modeling Meets Rift Analysis - A Numerical Modeling Study from the Jeanne d’Arc Basin, Offshore Newfoundland, and Canada. Marine and Petroleum Geology, 27(3), 585–99.
[13] BEHA, A., THOMSEN, R.O., & LITTKE, R., 2008, “A Rapid Method of Quantifying the -Flow Estimates in Basin Models.” 31(April):167–78.
[14] BLANC, E.P., ALLEN, M.B., INGER, S., & HASSANI, H., 2003, Structural styles in the Zagros simple folded zone, Iran. Journal of the Geological Society, 160(3), 401-412.
[15] BORDENAVE, M.L. & HERGE, J. A., 2005, “The influence of tectonics on the entrapment of oil in the Dezful Embayment, Zagros Foldbelt, Iran”, Journal of Petroleum Geology, 28(4), 339-368.
[16] FURST, M., 1990, “Strike-Slip Faults and Diapirism of the South-Eastern Zagros Ranges.” 149–82.
[17] HAKIMI, M.H., ASKAR NAJAF, A. ABDULA, R.A. and MOHIALDEEN, I., 2017, Generation and Expulsion History of Oil-Source Rock (Middle Jurassic Sargelu Formation) in the Kurdistan of North Iraq, Zagros Folded Belt: Implications from 1D Basin Modeling Study. Journal of Petroleum Science and Engineering, 162, 852–72.
[18] Hantschel T. and Kauerauf I. 2009. Fundamentals of Basin and Petroleum Systems Modeling.
[19] JACKSON, J., and MADINGLEY, R., 1981, Basement Faulting and the Focal Depths of the Larger Earthquakes in the Zagros Mountains (Iran), 561–86.
[20] JAMES, G.A., WYND, J.G., 1965, Stratigraphic Nomenclature of Iranian Oil Consortium Agreement Area: AAPG Bulletin 49, 2182–2245.
[21] JASSIN, S.Z and GOFF, J.C., 2006, Geology of Iraq; Dolin, Brno, distributed by Geol Soc. London, 232–250.
[22] Karimi A.R. Rabbani A.R. and Kamali M.R. (2016) “A bulk kinetic, burial history and thermal modeling study of the Albian Kazhdumi and the Eocene-Oligocene Pabdeh formations in the Ahvaz anticline, Dezful Embayment, IraN, Journal of Petroleum Science and Engineering, 146, pp 61-70.
[23] KARIMI A.R. RABBANI, A.R. KAMALI, M.R. and HEIDARFARD. M.H., 2016, Geochemical evaluation and thermal modeling of the Eocene–Oligocene Pabdeh and Middle Cretaceous Gurpi Formations in the northern part of the Dezful Embayment”, Arabian Journal of Geosciences, 432, pp 1-16.
[24] KOBRAEI, M., SADOUNI, J., & RABBANI, A.R., 2019, Organic geochemical characteristics of Jurassic petroleum system in Abadan Plain and north Dezful zones of the Zagros basin, southwest Iran. Journal of Earth System Science, 128(3), 50.
[25] MOUTHEREAU, F., LACOMBE, O., & VERGES, J., 2012, Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence. Tectonophysics, 532, 27-60.
[26] NOETH, S.R. THOMSON, O. and LITTKE, R., 2002, A Method for Assessing Statistical Significance and Uncertainties for Calibration of 1-D Thermal Basin Maturation Models. The American Association of Petroleum Geologists 3(3), 417–31.
[27] SABERI, M.H., RABBANI, A.R. & GHAVIDEL-SYOOKI, M., 2016, Hydrocarbon potential and palynological study of the Latest Ordovician–Earliest Silurian source rock (Sarchahan Formation) in the Zagros Mountains, southern Iran. Marine and Petroleum Geology, 71, 12-25.
[28] SEPEHR, M. and COSGROVJ.W., 2005, Role of the Kazerun Fault Zone in the formation and deformation of the Zagros fold-thrust belt, Iran, Tectonics, 24, 1–13.
[29] VERSFELT, P.L., 2001, AAPG Memoir 74, Chapter 21: Major Hydrocarbon Potential in Iran.
[30] YULKER, A. CORNFORD, C. and WELTE D., 1978, One-Dimensional Model to Simulate Geologic, Hydrodynamic and Thermodynamic Development of a Sedimentary Basin. Geologische Rundschau 67(3), 960–79.