Abstract
Assessment of conditions that favoured hydrocarbon accumulations necessitates sedimentological characterization and facies identification as it elucidates the detailed records of the depositional environment and its evolution. Integration of various data sources becomes imperative for the establishment of the facies architecture which enables the evaluation of reservoir quality for Jubilee field in the deep Tano Basin. Early stage realization of decrease in production prediction of the field was attributed to early water breakthrough, baffle bridges and reservoir heterogeneity. This development requires its sedimentological evaluation through textural characterization, lithofacies identification and reservoir quality indication. The identified seventeen lithofacies allowed the deduction of deep-marine turbidite depositional environment. Our findings highlight the significance of sedimentological and facies development processes in the overall evolution of deep-water channel systems. The history of the Jubilee channel complex sets almost definitely characterizes many other emerging undersea channel systems and can be used to evaluate the distribution, shape, and structuring of the resulting reservoir sands. In turn, the Jubilee data set adds to the library of channel-levee-splay-lobe systems, aids as a prospective predictive model for hydrocarbon exploration and development, and as an outcrop explanatory analogue of a channel-splay system.
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References
Ahmed MJ (2021) Microfacies analysis and depositional development of Shuaiba formation in the West Qurna oil field, Southern Iraq. Model Earth Syst Environ 7(4):2697–2707. https://doi.org/10.1007/s40808-020-01036-w
Ali SK, Janjuhah HT, Shahzad SM, Kontakiotis G, Saleem MH, Khan U, Zarkogiannis SD, Makri P, Antonarakou A (2021) Depositional sedimentary facies, stratigraphic control, paleoecological constraints, and paleogeographic reconstruction of late Permian Chhidru Formation (Western Salt Range, Pakistan). J Mar Sci Eng 9(12):1372. https://doi.org/10.3390/jmse9121372
Al-Mimar HS, Awadh SM, Al-Yaseri AA, Yaseen ZM (2018) Sedimentary units-layering system and depositional model of the carbonate Mishrif reservoir in Rumaila oilfield, Southern Iraq. Model Earth Syst Environ 4(4):1449–1465. https://doi.org/10.1007/s40808-018-0510-5
Antobreh AA, Faleide JI, Tsikalas F, Planke S (2009) Rift–shear architecture and tectonic development of the Ghana margin deduced from multichannel seismic reflection and potential field data. Mar Pet Geol 26(3):345–368. https://doi.org/10.1016/j.marpetgeo.2008.04.005
Atta-Peters D, Agama CI, Asiedu DK, Apesegah E (2013) Palynology, palynofacies and palaeoenvironments of sedimentary organic matter from Bonyere-1 Well, Tano basin, Western Ghana. Int Lett Nat Sci 5:27–45
Azidane H, Michel B, Bouhaddioui ME, Haddout S, Magrane B, Benmohammadi A (2021) Grain size analysis and characterization of sedimentary environment along the Atlantic Coast, Kenitra (Morocco). Mar Georesour Geotechnol 39(5):569–576. https://doi.org/10.1080/1064119X.2020.1726536
Bempong FK, Ehinola O, Apesegah E, Hotor VK, Botwe K (2021a) Sequence Stratigraphic Framework, Depositional Settings and Hydrocarbon Prospectivity of the Campanian Section, Tano Basin Southwestern Ghana. Petrol Coal 63(1):204–215
Bempong FK, Mensah CA, Bate BB, Abdul RM, Akaba PA (2021b) Seismic chronostratigraphic illustration of the Tertiary Section in Tano Basin Southwestern Ghana. Petrol Coal 63(3):742–750
Bouma AH (1962) Sedimentology of some flysch deposits: a graphic approach to facies interpretation. Elsevier, Amsterdam, p 168
Dailly P, Henderson T, Hudgens E, Kanschat K, Lowry P (2013) Exploration for Cretaceous stratigraphic traps in the Gulf of Guinea, West Africa and the discovery of the Jubilee field: a play opening discovery in the Tano Basin, Offshore Ghana. Geol Soc Lond Spec Publ 369(1):235–248. https://doi.org/10.1144/SP369.12
Donselaar ME, Schmidt JM (2005) Integration of outcrop and borehole image logs for high-resolution facies interpretation: example from a fluvial fan in the Ebro Basin Spain. Sedimentology 52(5):1021–1042. https://doi.org/10.1111/j.1365-3091.2005.00737.x
El-Tehiwy AA, El-Anbaawy MI, Rashwan NH (2019) Significance of core analysis and gamma-ray trends in depositional facies interpretation and reservoir evaluation of Cenomanian sequence, Alam El-Shawish East Oil Field, North Western Desert Egypt. J King Saud Univ Sci 31(4):1297–1310. https://doi.org/10.1016/j.jksus.2018.12.002
Farrell KM, Harris WB, Mallinson DJ, Culver SJ, Riggs SR, Wehmiller JF, Moore JP, Self-Trail JM, Lautier JC (2013) Graphic logging for interpreting process-generated stratigraphic sequences and aquifer/reservoir potential: with analog shelf to shoreface examples from the Atlantic Coastal Plain Province, USA. J Sediment Res 83(8):723–745. https://doi.org/10.2110/jsr.2013.52
Folk RL, Ward WC (1957) Brazos River bar [Texas]; a study in the significance of grain size parameters. J Sediment Res 27(1):3–26. https://doi.org/10.1306/74D70646-2B21-11D7-8648000102C1865D
Friedman GM (1961) Distinction between dune, beach, and river sands from their textural characteristics. J Sediment Res 31(4):514–529. https://doi.org/10.1306/74D70BCD-2B21-11D7-8648000102C1865D
Friedman GM (1967) Dynamic processes and statistical parameters compared for size frequency distribution of beach and river sands. J Sediment Res 37(2):327–354. https://doi.org/10.1306/74D716CC-2B21-11D7-8648000102C1865D
Ghaznavi AA, Quasim MA, Ahmad AHM, Ghosh SK (2019) Granulometric and facies analysis of Middle-Upper Jurassic rocks of Ler Dome, Kachchh, western India: an attempt to reconstruct the depositional environment. Geologos. https://doi.org/10.2478/logos-2019-0005
Huang W, Li S, Chen H, Fu C (2020) A river-dominated to tide-dominated delta transition: a depositional system case study in the Orinoco heavy oil belt, Eastern Venezuelan Basin. Mar Pet Geol 118:104389. https://doi.org/10.1016/j.marpetgeo.2020.104389
Islam AT, Shuanghe S, Islam MA, Sultan-ul-Islam M (2017) Paleoenvironment of deposition of Miocene succession in well BK-10 of Bengal Basin using electrofacies and lithofacies modeling approaches. Model Earth Syst Environ 3(1):5. https://doi.org/10.1007/s40808-017-0279-y
Kolla V (2007) A review of sinuous channel avulsion patterns in some major deep-sea fans and factors controlling them. Mar Petrol Geol 24:450–469. https://doi.org/10.1016/j.marpetgeo.2007.01.004
Lowe DR (1982) Sediment gravity flows: II. Depositional models with special reference to the deposits of high-denisty turbidity currents. J Sediment Petrol 52:279–297. https://doi.org/10.1306/212F7F31-2B24-11D7-8648000102C1865D
Lowe DR, Graham SA, Malkowski MA, Das B (2019) The role of avulsion and splay development in deep-water channel systems: sedimentology, architecture, and evolution of the deep-water pliocene Godavari “A” channel complex, India. Mar Pet Geol 105:81–99. https://doi.org/10.1016/j.marpetgeo.2019.04.010
Moiola RJ, Weiser D (1968) Textural parameters; an evaluation. J Sediment Res 38(1):45–53
Omisore BO, Fayemi O, Brantson ET, ** S, Ansah E (2022) Three-dimensional anisotropy modelling and simulation of gas hydrate borehole-to-surface responses. J Nat Gas Sci Eng 106:104738. https://doi.org/10.1016/j.jngse.2022.104738
Pacheco F, Harrison M, Chatterjee S, Ishinaga K, Ishii S, Mills W, Vargas N, Paul S, Roy P (2019) Integrated sedimentological and seismic reservoir characterization studies as inputs into a Lower Cretaceous reservoir geomodel, offshore Abu Dhabi. First Break 37(10):73–84. https://doi.org/10.3997/1365-2397.2019027
Pattison SA (2019) Re-evaluating the sedimentology and sequence stratigraphy of classic Book Cliffs outcrops at Tusher and Thompson canyons, eastern Utah, USA: applications to correlation, modelling, and prediction in similar nearshore terrestrial to shallow marine subsurface settings worldwide. Mar Pet Geol 102:202–230. https://doi.org/10.1016/j.marpetgeo.2018.12.043
Radwan AE (2021) Modeling the depositional environment of the sandstone reservoir in the Middle Miocene Sidri Member, Badri Field, Gulf of Suez Basin, Egypt: Integration of gamma-ray log patterns and petrographic characteristics of lithology. Nat Resour Res 30(1):431–449. https://doi.org/10.1007/s11053-020-09757-6
Rajganapathi VC, Jitheshkumar N, Sundararajan M, Bhat KH, Velusamy S (2013) Grain size analysis and characterization of sedimentary environment along Thiruchendur coast, Tamilnadu India. Arab J Geosci 6(12):4717–4728. https://doi.org/10.1007/s12517-012-0709-0
Rüpke LH, Schmid DW, Hartz EH, Martinsen B (2010) Basin modelling of a transform margin setting: structural, thermal and hydrocarbon evolution of the Tano Basin Ghana. Petrol Geosci 16(3):283–298. https://doi.org/10.1144/1354-079309-905
Shahbazi A, Monfared MS, Thiruchelvam V, Fei TK, Babasafari AA (2020) Integration of knowledge-based seismic inversion and sedimentological investigations for heterogeneous reservoir. J Asian Earth Sci 202:104541. https://doi.org/10.1016/j.jseaes.2020.104541
Shukla UK (2009) Sedimentation model of gravel-dominated alluvial piedmont fan, Ganga Plain India. Int J Earth Sci 98(2):443–459. https://doi.org/10.1007/s00531-007-0261-4
Siddiqui NA, Ramkumar M, Rahman AHA, Mathew MJ, Santosh M, Sum CW, Menier D (2019) High resolution facies architecture and digital outcrop modeling of the Sandakan formation sandstone reservoir, Borneo: implications for reservoir characterization and flow simulation. Geosci Front 10(3):957–971. https://doi.org/10.1016/j.gsf.2018.04.008
Siddiqui NA, Mathew MJ, Ramkumar M, Sautter B, Usman M, Rahman AHA, El-Ghali MA, Menier D, Shiqi Z, Sum CW (2020) Sedimentological characterization, petrophysical properties and reservoir quality assessment of the onshore Sandakan Formation, Borneo. J Petrol Sci Eng 186:106771. https://doi.org/10.1016/j.petrol.2019.106771
Solórzano EJ, Buatois LA, Rodríguez WJ, Mángano MG (2021) Sedimentary facies of a tide-dominated estuary and deltaic complex in a tropical setting: the middle Miocene Oficina Formation of the Orinoco Oil Belt, Venezuela. J S Am Earth Sci 112:103515. https://doi.org/10.1016/j.jsames.2021.103515
Spencer DW (1963) The interpretation of grain size distribution curves of clastic sediments. J Sediment Res 33(1):180–190. https://doi.org/10.1306/74D70DF8-2B21-11D7-8648000102C1865D
Stow D, Smillie Z (2020) Distinguishing between deep-water sediment facies: turbidites, contourites and hemipelagites. Geosciences 10(2):68. https://doi.org/10.3390/geosciences10020068
Su M, Luo K, Fang Y, Kuang Z, Yang C, Liang J, Liang C, Chen H, Lin Z, Wang C, Lei Y (2021) Grain-size characteristics of fine-grained sediments and association with gas hydrate saturation in Shenhu Area, northern South China Sea. Ore Geol Rev 129:103889. https://doi.org/10.1016/j.oregeorev.2020.103889
Tan MT, Van Thuan D, Dy ND, Van Tao N, Ha TTT, Dao NT (2019) Environments of upper miocene sediments in the Hanoi depression interpreted from grain-size parameters Vietnam. J Earth Sci 41(2):182–199. https://doi.org/10.15625/0866-7187/41/2/13798
Tullius DN, Leier AL, Galloway JM, Embry AF, Pedersen PK (2014) Sedimentology and stratigraphy of the Lower Cretaceous Isachsen Formation: Ellef Ringnes Island, Sverdrup Basin, Canadian Arctic Archipelago. Mar Pet Geol 57:135–151. https://doi.org/10.1016/j.marpetgeo.2014.05.018
Xu Z, Plink-Björklund P, Wu S, Liu Z, Feng W, Zhang K, Yang Z, Zhong Y (2022) Sinuous bar fingers of digitate shallow-water deltas: Insights into their formative processes and deposits from integrating morphological and sedimentological studies with mathematical modelling. Sedimentology 69(2):724–749. https://doi.org/10.1111/sed.12923
Boggs S (2012) Principles of sedimentology and stratigraphy
Martinius AW, Hegner J, Kaas I, Bejarano C, Mathieu X and Mjos R (2013). Geologic reservoir characterization and evaluation of the Petrocedeno field, early Miocene Oficina Formation, Orinoco heavy oil belt, Venezuela. https://doi.org/10.1306/13371590St643559
Acknowledgements
We gratefully acknowledge Mr Michael Aryeetey, (Exploration and Appraisal Manager). Mr Ebenezer Apesegah (Geology Manager) and Mr Mark Prempeh (Deputy Manager) of Ghana National Petroleum Corporation for providing access to data for this research and for granting permission to publish the paper. The authors would also like to thank anonymous reviewers for their contributions to this research. Finally, we thank the University of Mines and Technology, Tarkwa, Ghana, and the Petroleum Geosciences and Engineering Department for the financial support through the Getfund Scholarship.
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EA: formal analysis, investigation, writing—original draft. AE: editing, formal analysis and supervision. ETB: editing, formal analysis and supervision. JSYK: editing, formal analysis and supervision. SAO: editing, formal analysis and supervision. BKO: editing, formal analysis and supervision. CN: editing, formal analysis and supervision.
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Ansah, E., Ewusi, A., Brantson, E.T. et al. Sedimentological and facies characterization in the modelling of the Turonian sandstone reservoir package, Jubilee field, Ghana. Model. Earth Syst. Environ. 9, 1135–1168 (2023). https://doi.org/10.1007/s40808-022-01550-z
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DOI: https://doi.org/10.1007/s40808-022-01550-z