Diagenetic Effects and Porosity Evolution of Zubair Formation in West Qurna Oil Field, Southern Iraq

Authors

  • Rusul Hakim Ali Department of Geology, College of Science, University of Baghdad, Iraq
  • Aiad Ali Hussien Al-Zaidy Department of Geology, College of Science, University of Baghdad, Iraq.

DOI:

https://doi.org/10.48165/

Keywords:

Diagenetic Effects, Porosity Evolution, Zubair Formation, West Qurna Oil Field, Southern Iraq

Abstract

This present study includes the petrography, lithofacies analysis and depositional development for the  Zubair Formation in six boreholes (WQ-1, WQ-13, WQ-15, WQ-60, WQ-148 and WQ-356) within  the West Qurna oil field. Zubair Formations was deposited within Mesopotamian Zone during the  Barremain stage which belongs to the Early Cretaceous epoch. The Zubair formation in the study area  affected by many diagenetic processes through and after the deposition. There are three diagenetic  zones in this succession; the lower part of the Zubair Formation is characterized with three effected  porous zone, which is separated by high compacted and cemented sandstone. The middle part of this  formation is showing high compacted sandstone with appeared the overgrowth quartz and micro quartz cementation. While the upper Zubair Formation is affected by compaction shale alternative  with high compaction overgrowth quartz. The quartz arenite sandstone affected by the compaction in  low amount follows by chemical dissolution led to made the secondary quartz precipitated on the  original grains this decrease the primary porosity, the increase of compaction process destroyed the quartz and rock fragment grains this associated with chemical solution which led to precipitate extra  grains of quartz as a small grain decreasing the porosity. After this process the changing in chemical  and physical properties of depositional basin led to precipitate the calcite cement, and finally as results  of organism activity calcite were dissolved and produced the secondary porosity. The effective porosity  values distribution in the studied succession, where appeared in the lower unit one moderate  permeable zone in all studied wells separated by impermeable zone in WQ-60 to became two zone.  Whiles the middle unit characterized by two moderate and two high permeable zones. The first  moderate zone is appeared in the lower part of middle unit within WQ-60 , 15 and 1, while the second  is appeared in the upper part of this unit within WQ-15, 1 and 356.The upper unit is showing one  limited moderate permeable zone within WQ-60 and 15. 

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References

Ali R. H. and Al-Zaidy A. A. (2020). Lithofacies Analysis and Depositional Development of Zubair Formation in West Qurna Oil Field, Southern Iraq. Journal of University of Babylon for Pure and Applied Sciences, 28(3).

Al-Zaidy A. A. (2019). Facies Analysis and Sequence Stratigraphy of the Zubair Formation in the Kifl oil field, Central of Iraq. Iraqi Journal of Science, 60(2), 341-352.

Al-Zaidy A. A. (2020). Facies architecture and stratigraphic sequence of Zubair Formation in Majnoon and Suba oil fields, Southern Iraq. Modeling Earth Systems and Environment, 6, 779–792.

Al-Zaidy A. A., Sattam M., Nasir M. E., (2013). High Resolution Sequence Stratigraphy and Reservoir Characterization of the Hartha Formation in Ahdab Oilfield. Journal of Babylon University Engineering Sciences, 21(1), 37- 49.

Aqrawi, A. A. M., Goff, J. C., Horbury, A.D. and Sadooni, F.N. (2010). The petroleum Geology of Iraq. Scientific Press Ltd., 424pp.

Asquith, G. and Gibson, C. (1982). Basic well log analysis for geologists: methods in Exploration series, AAPG, 216p.

Boggs, S. J. (1995). Principles of Sedimentology and Stratigraphy, Prentice Hall, New Jersey, U.S.A., 774P.

Burley, S. D. (1984). Patterns of diagenesis in the Sherwood Sandstone Group (Triassic), United Kingdom. Clay Minerals, 19, 403–440

Choquette P.W. and Pray L.C. (1970). Geological nomenclature and classification of porosity in sedimentary carbonate. APGB, 54, 207- 250.

Folk, R. L. (1968) Petrology of Sedimentary Rocks. Austin TX: University of Texas Publication, 76.

Jassim S. Z. and Goff J. C. (2006). Geology of Iraq .Dolin, Prague and Moravian Museum, Brno. pp: 341.

Jassim, S. Z. and Al-Gailani, M., (2006). Hydrocarbons. In: Jassim, S.Z. and Goff, J.C. (Eds), Geology of Iraq. Dolin, Prague and Moravian Museum, Brno, Czech Republic, pp.232-250.

Krynine, P. D. (1946). Microscopic morphology of quartz types: Anals do Segundo Congr. Panamericano de Engenharia de Minas e Geol., 3, 35-49.

Moore, C. H. (1989). Carbonate Diagenesis and Porosity: Elsevier Publ. Co., Developments in Sedimentology 46, 338 p.

Scholle, P. A. (1981). A Color Illustrated Guide to Constituents, Textures, Cements, and Porosities of Sandstones and Associated Rocks, The American of Petroleum Geologists with the support of The American Association Petroleum Geologists Foundation, Tulsa, Oklahoma, U.S.A.

Selley, R. C. (2000). Applied Sedimentary (2nd Ed.); Academic Press, London, 523P. 17. Summerfield, M.A., 1983. Silcrete. In: Goudie, A.S., Pye, K., Guthrie, G.D., Mossman, B.T. (Eds), Chemical Sediments and Geomorphology. Academic Press, London, 59-61.

Surdam R.C., Crossly L.J., Hagen E.S. and Heasler H.P. (1989). Organic-Inorganic Interactions and Sandstone Diagenesis.

The American Association of Petroleum Geologists Bulletin, 73(1), 1-2.

Worden R. H. and Burley S. D. (2003). Sandstone diagenesis: the evolution of sand to stone. Sandstone Diagenesis: Recent and Ancient Edited by Stuart D. Burley and Richard H. Worden. International Association of Sedimentologists. ISBN: 978-1-405-10897- 3.

Wright, T. O. and L. B. Platt. (1982). Pressure dissolution and cleavage in Martingsburg shale. American Journal of Science, 282, 122-135.

Published

2021-12-15

How to Cite

Ali, R.H., & Al-Zaidy, A.A.H. (2021). Diagenetic Effects and Porosity Evolution of Zubair Formation in West Qurna Oil Field, Southern Iraq . Bulletin of Pure and Applied Sciences-Geology , 40(2), 154–170. https://doi.org/10.48165/