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Structural Analysis of Bornu Basin, Northeastern Nigeria Based on Coherence and Curvature Attributes
Umeghalu C.O.1 , Egwuonwu G.N.2
- Physics and Industrial Physics, Nnamdi Azikiwe University, Awka, Nigeria.
- Physics and Industrial Physics, Nnamdi Azikiwe University, Awka, Nigeria.
Section:Research Paper, Product Type: Journal-Paper
Vol.9 ,
Issue.7 , pp.1-6, Jul-2023
Online published on Jul 31, 2023
Copyright © Umeghalu C.O., Egwuonwu G.N. . This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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IEEE Style Citation: Umeghalu C.O., Egwuonwu G.N., “Structural Analysis of Bornu Basin, Northeastern Nigeria Based on Coherence and Curvature Attributes,” International Journal of Scientific Research in Multidisciplinary Studies , Vol.9, Issue.7, pp.1-6, 2023.
MLA Style Citation: Umeghalu C.O., Egwuonwu G.N. "Structural Analysis of Bornu Basin, Northeastern Nigeria Based on Coherence and Curvature Attributes." International Journal of Scientific Research in Multidisciplinary Studies 9.7 (2023): 1-6.
APA Style Citation: Umeghalu C.O., Egwuonwu G.N., (2023). Structural Analysis of Bornu Basin, Northeastern Nigeria Based on Coherence and Curvature Attributes. International Journal of Scientific Research in Multidisciplinary Studies , 9(7), 1-6.
BibTex Style Citation:
@article{C.O._2023,
author = {Umeghalu C.O., Egwuonwu G.N.},
title = {Structural Analysis of Bornu Basin, Northeastern Nigeria Based on Coherence and Curvature Attributes},
journal = {International Journal of Scientific Research in Multidisciplinary Studies },
issue_date = {7 2023},
volume = {9},
Issue = {7},
month = {7},
year = {2023},
issn = {2347-2693},
pages = {1-6},
url = {https://www.isroset.org/journal/IJSRMS/full_paper_view.php?paper_id=3197},
publisher = {IJCSE, Indore, INDIA},
}
RIS Style Citation:
TY - JOUR
UR - https://www.isroset.org/journal/IJSRMS/full_paper_view.php?paper_id=3197
TI - Structural Analysis of Bornu Basin, Northeastern Nigeria Based on Coherence and Curvature Attributes
T2 - International Journal of Scientific Research in Multidisciplinary Studies
AU - Umeghalu C.O., Egwuonwu G.N.
PY - 2023
DA - 2023/07/31
PB - IJCSE, Indore, INDIA
SP - 1-6
IS - 7
VL - 9
SN - 2347-2693
ER -
Abstract :
The Bornu Basin, extending into Chad Republic, Cameroon, and Niger Republic, is a basin formed through the mechanical separation of the African crustal plate during the Cretaceous period. The study area encompasses Latitude 11.750 N to 13.000 N and Longitude 12.000 E to 14.000 E. Structural analysis of the Bornu Basin utilized coherence and curvature attributes to examine the technique offering the best structural resolution and to understand the various structural styles present in the basin. The integration of 3-D seismic data and well data was employed for this purpose. The findings indicate that while the coherence attribute and the curvature attribute display similar comparisons in terms of frequency and gradient readings, the coherence attribute provides higher resolution when examining smaller structures. This demonstrates its superior effectiveness in visualizing structural trends within the basin. Additionally, the results revealed the presence of several types of faults, ranging from deep-lying mega faults that extend down to the basement, to micro faults that do not reach the basement. These faults can serve as both hydrocarbon seals and potential pathways for hydrocarbon migration.
Key-Words / Index Term :
Coherence, Curvature, Variance, Seismic Attribute, Faults, Anticline, Seismic Horizon, Anomaly.
References :
[1] A. A. Avbovbo, E. O. Ayoola and S. A. Osahon, “Depositional and structural styles in Chad Basin of Northeastern Nigeria”, AAPG, Vol. 70, Issue 121, pp.1787–1798, 1986.
[2] C. F. Ezeobi, G. N. Egwuonwu and I.U. Chibuogwu. “Reservoir Identification in Bornu Basin, Northeastern Nigeria Based on Well Log Analysis”, International Journal of Scientific Research in Physics and Applied Sciences, Vol. 11, Issue 1, pp. 7-16. 2023a.
[3] N. G. Obaje, H. Wehner and G. Scheeder, “Hydrocarbon prospectivity of Nigeria’s inland basins: From the viewpoint of organic geochemistry and organic petrology”, AAPG Bulletin, 2004, Vol. 87, PP.325–353, 2004
[4] I. Hamza and I. Hamidu, “Hydrocarbon resource potential of the Bornu basin northeastern Nigeria”, Global Journal of Geological Sciences, 10(1), 2012.
[5] S. P. Braide, “Petroleum geology of the southern Bida Basin Nigeria”, American Association of Petroleum Geologists, Vol. 74, Issue 5, pp. 717 - 725, 1990.
[6] G. J. Genik “Regional framework structure and petroleum aspects of the rift basins in Niger, Chad and Central African Republic (C.A.R.)”, Tectonophysics, Vol. 213, pp.169–185, 1992.
[7] C. O. Ajayi and D. E. Ajakaiye, “The Origin and Peculiarities of the Nigeria Benue Trough. Another look from recent gravity data obtained from middle Benue”, Tectonophysics, Vol.12, pp.286-329, 1981.
[8] NGSA, “Geological and Mineral Resources Map Album”, Nigerian Geological Survey Agency, 2006.
[9] C. F. Ezeobi, G. N. Egwuonwu and I.U. Chibuogwu, “Reservoir Identification in Bornu Basin, Northeastern Nigeria Using Seismic Attributes Analysis”. International Journal of Scientific Research in Multidisciplinary Studies, 9 (2), pp 1-8, 2023b.
[10] S. W. Petter and C. M. Ekweozor, “petroleum Geology of Benue Trough and southeastern Chad Basin Nigeria”, GEOLOGIC NOTES, AAPG Bulletin 66, 1141-1149, 1982.
[11] K. O. Omosanya, A. A. Akinmosin and N. A. Adio, “Hydrocarbon potential of the Nigerian chad basin from wireline logs”, Indian Journal of Science, Vol. 4, Issue 12, pp.1668-1675, 2011.
[12] C. N. Nwankwo and A. S. Ekine, “ Geothermal gradients in the Chad basin, Nigeria from bottom hole temperature logs, Int Journal of Physical Sciences, Vol. 4, Issue 12, pp. 777-783, 2009.
[13] J. A. Adeyinka, S. P. Ola and S. O. Olabode, “Possible Bornu Basin Hydrocarbon Habitat”, International Journal of Geoscience, Vol.5, Issue 9, 2014.
[14] S. A. Aminu and M. Whiteworth, “Integrated well log and 2-D seismic data interpretation to image subsurface stratigraphy and structure in Northeastern Bornu Basin”, Journal of African Earth Science, Vol. 121, pp. 1 – 15, 2016
[15] S. K. Ahmed, K. Liu, H. Moussa, J. Liu, A. H. Ahmed and L. K. Kra, “Assessment of petroleum system elements and migration pattern of Borno (Chad) Basin, Northeastern Nigeria”, Journal of petroleum science and engineering, Vol. 208, 2022.
[16] C. N. Didi, I. I. Obiadi, S. E. Okeke, S. N. Anakor and M. K. Ikomi, “Lithostratigraphic interpretation and analysis of the depositional environment of Nigerian Chad basin using well log and seismic data”, Meridian Journal of Physical Science, Vol. 2, Issue 1, 2022.
[17] S. Chopra and J. M. Kurt, “Seismic attributes—A historical perspective”, Geophysics, Vol. 70, Issue 5, pp.3SO?28SO, 2005.
[18] M. T. Taner, “Seismic attributes”, CSEG Recorder, September, pp. 48–56, 2001.
[19] M. Bahorich and S. Famer, “3D seismic discontinuity for faults and stratigraphic features, the coherence cube” Leading Edge, Vol. 14, Issue 10, pp. 1053-1058, 1995.
[20] K. D. Opeyemi and A. P. Aizebeokhai “Seismic attribute analysis for reservoir characterization, offshore Niger delta”, Petroleum and Coal, Vol. 57, Issue 6, pp. 619 – 628, 2016.
[21] R. J. Lisle, “Detection of zones of abnormal strains in structures using Gaussian curvature analysis”, AAPG Bulletin, Vol. 78, pp. 1811-1819, 1994.
[22] A. R. Brown, “Understanding seismic attributes”, Geophysics, Vol. 66: 47-48, 2001.
[23] M. T. Taner, J. S. Schuelke, R. O. Doherty, and E. Baysal, “Seismic attributes revisited”, expanded abstract, society of exploration geophysicists, 1995.
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