Abstract
Hydrocarbon generation potential and porosity types of the Middle Triassic Geli Khana Formation in Jabal Kand-1 (JK-1) well and from outcrop section at Ora of northern Iraq are investigated. Total organic carbon, pyrolysis, and maturation assessment such as thermal alteration index (TAI) and vitrinite reflectance (Ro%) for 19 shale samples are conducted. The analyses showed a sufficient amount of organic matter (OM) occurs in JK-1 specifically. According to the obtained samples from the pyrolysis analysis of the studied samples, the existing organic matters in well (JK-1) are composed of a mixed of kerogen type II–III and III; while type IV in outcrop section which found in post mature state, indicating dry gas window. The estimated TAI for the studied section ranged between 3.3 in and 3.7 in JK-1 and 3.3–4 in Ora section. Additionally, the maturity derived information from vitrinite reflectance supported that the Geli Khana Formation is in dry gas window and post mature stage in both sections due to the average ratio of (Ro %) which is between 1.35 and 2 %. The porosity types in the carbonate successions of the formation include; fracture, moldic, intergranular, intramatrix, vuggy, intercrystalline, channel and fenestral birds-eye porosities. These types enhance the reservoir characteristics of the carbonate succession of the formation.
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References
Abboud MS (1995) Metallic elements in Triassic petroleum. Research Journal of Allepo University, Syria
Abboud MS (1996) Vanadium and its relationship to the heavy fractions in Syrian oils. Research Journal of Allepo University, Syria 11:1–1
Abboud M, Philp RP, Allen J (2005) Geochemical correlation of oils and source rocks from central and NE Syria. Journal of Petroleum Geology 28:203–216
Akinlua A, Ajayi TR, Jarvie DM, Adeleke BB (2005) A reappraisal of the application of Rock Eval Pyrolysis to Source Rock studies in the Niger Delta. Journal of Petroleum Geology 28:39–48
Al-Adool DMH (1998) Sedimentary facies and depositional environments of Triassic rock (Sythian-Carnian) North West Iraq. Mosul University, Iraq, PhD Dissertation
Alsharhan AS, Nairn AEM (1997) Sedimentary basins and petroleum geology of the Middle East. Elsevier, Amsterdam
Aqrawi AM, Horbury AD, Goff JC, Sadooni FN (2010) The Petroleum Geology of Iraq, Scientific Press
Archie GE (1952) Classification of carbonate reservoir rocks and petrophysical considerations. AAPG Bulletin 36:278–298
Ascaso C, Wierzchos J, Corral JC, Lopez R, Alonso J (2003) New applications of light and electron microscopic techniques for the study of microbiological inclusions in amber. Journal of Paleontology 77:1182–1192
Barker C (1996) Thermal modeling of petroleum generation: theory and applications. Elsevier, New York; Amsterdam
Bein A, Gvirtzman G (1977) A Mesozoic edge of the Arabian Plate along the Levant coastline and its bearing on the evolution of the eastern Mediterranean. Structural History of the Mediterranean Basins, Editions Technip, Paris
Brooks J (1981) Organic maturation of sedimentary organic matter, à review. In: Brook J (ed) Organic maturation studies and fossil fuel exploration. Academic, London
Buday T (1980) The regional geology of Iraq, vol 1. Stratigraphy and pale geography, Dar Al-Kutub publishing house, university of Mosul, Iraq
Buday T, Jassim SZ (1987) The regional geology of Iraq. Tectonism, Magmatism and Metamorphism. State Establishment of Geological Survey and Mineral Investigation, Baghdad, Iraq
Choquette PW, Pray LC (1970) Geologic nomenclature and classification of porosity in sedimentary carbonates. AAPG Bulletin 54:207–244
Douban A F, Al-Sahlan G, Fenton JPG (2001) Sequence stratigraphic distribution and biostratigraphic zonation of the Permo-Triassic Section in Kuwait: American Association of Petroleum Geologists Bulletin, v. 85
Espitalie J, Madec M, Tissot BP, Menning JJ, Leplat P (1977) Source rock characterization method for exploration, Offshore Techn. Conf. Paper 2935, 11th Annual OTC, Houston
Ghiorse WC, Ehrlich HL (1992) Microbial mineralization of iron and manganese. Catena Supplement 21:75–99
Ghori KAK (2002) Modeling the hydrocarbon generative history of the Officer Basin. Western Australia, PESA Journal 29:29–42
Hall PK (1957) The geology of Rikan and Zibar, manuscript report. GEOSURV, Baghdad, Iraq
Hunt JM (1996) Petroleum geochemistry and geology (second edition). freeman and company, New York
Jassim SZ, Buday T (2006) Units of the unstable shelf and the Zagros suture. In: Jassim SZ, Goff J (eds) Geology of Iraq, Dolin, Prague, and Moravian Museum. Czech Republic, Brno, pp 71–83
Martini AM, Budai JM, Walter LM, Schoell M (1996) Microbial generation of economic accumulations of methane within a shallow organic-rich shale. Nature 383:155–158
Mason GM (2008) Eocene age fossilized filamentous bacteria: new evidence suggesting a bacterial genesis of siderite in the Green River Formation, Wyoming. Proceedings of the 28th Oil Shale Symposium, Colorado School of Mining, pp.1-7
Mason GM, Kirchner G (1994) Bacterial influence upon the deposition of siderite. Green River Formation, Wyoming, In: Proceedings of the (1993) Eastern Oil Shale Symposium. Institute for Mining and Minerals Research Lexington, Kentucky, pp 381–389
NOC (1983) Internal report, the final well report of JK-1 well, (unpublished report)
Nunez L, Baceta JI (1994) Basics and application of Rock-Eval/TOC Pyrolysis: an example from the uppermost Paleocene/lowermost Eocene in the Basque Basin, Western Pyrenees. MUNIBE (Ciencias Naturales - Natur Zientziak) San Sebastian 46:43–62
Pearson DL (1990) Pollen/spore color standed (Ver.2). Phillips Petroleum Company, Bartelsville
Peters KE (1986) Guidelines for evaluating petroleum source rock using programmed pyrolysis: American Association of Petroleum Geologists. Bull Am Meteorol Soc 70:318–329
Ponikarov VP (1967) The geology of Syria, explanatory notes on the geological map of Syria, scale 1:500,000, part1, Stratigraphy. Syrian Arab Republic, Ministry of Industry, Damascus, Igneous Rocks and Tectonics
Roadifer RE (1987) Size distributions of the world’s largest known oil and tar accumulations. In: Meyer RF (ed) Exploration for heavy crude oil and natural bitumen. AAPG Studies in Geology, vol 25. AAPG, Tulsa, Oklahoma, pp 3–23
Sadooni FN (1995) Petroleum prospects of the upper triassic carbonates in northern Iraq. Journal of Petroleum Geology 18:171–190
Sadooni FN, Alsharhan AS (2004) Stratigraphy, lithofacies distribution, and petroleum potential of the Triassic strata of the northern Arabian plate. AAPG Bulletin 88:515–538
Selley RC (1985) Elements of petroleum geology. Academic, London, UK
Serryea OA (1990) Geochemestry of organic matter and oil, oil and Arab cooperation
Setudehnia A (1978) The Mesozoic sequence in south-west Iran and adjacent areas. Journal of Petroleum Geology 1:3–42
Sharland PR, Archer R, Casey DM, Davies RB, Hall SH, Heward AP, Horbury AD, Simmons MD (2001) Arabian plate sequence stratigraphy. GeoArabia special publication 2, Gulf PetroLink, Bahrain
Tissot BP, Welte DH (1984) Petroleum Formation and occurrence: a new approach to oil and gas exploration, second edition. Springer, Berlin
Ziegler MA (2001) Late Permian to Holocene paleofacies evolution of the Arabian Plate and its hydrocarbon occurrences. GeoArabia 6:445–505
Acknowledgments
Special thanks are to go to the staff of North Oil Company for their assistance to proved samples. Thanks and respect is given to Dr. Alimi Hussein from Weathearford Laboratories—Texas for his cooperation in analyzing all samples. Thanks are due to Georg Oleschinski from Geological Institute of Bonn University/Germany for help in scanning electron microscopic study.
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Naqishbandi, S.F., Jabbar, W.J. & Al-Juboury, A.I. Hydrocarbon potential and porosity types of the Geli Khana Formation (Middle Triassic), Northern Iraq. Arab J Geosci 8, 739–758 (2015). https://doi.org/10.1007/s12517-013-1258-x
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DOI: https://doi.org/10.1007/s12517-013-1258-x