Determination of Hydrocarbon Potentials Using High Resolution Aeromagnetic Data over Sokoto Basin, Northwestern Nigeria
- 1 Department of Geology and Mining, Adamawa State University, Mubi, Nigeria
Abstract
Aeromagnetic method of exploration is famed for its suitability for locating buried magnetic ore bodies because of their magnetic susceptibility. This method has been used in the early stage of petroleum exploration to determine depth and major structures of crystalline Basement rocks underlying the sedimentary basin. In this study, high resolution aeromagnetic data were used to ascertain the viability for hosting hydrocarbon potentials of the study area which forms part of the Illummeden Basin (also known locally as the Sokoto embayment) of West Africa. This was largely carried out through Spectra analysis to determine sediment thickness. The results of the analysis of the aeromagnetic data show that, deeper magnetic source ranges from 0.41 km to 2.69 km, shallow magnetic sources from 0.17 km to 0.97 km. Areas with shallow sediment thickness could not allow the thermal maturation of the sediments, since temperature increase with depth and a depth of two kilometers and above has a temperature range of 60 ° C and above. Areas with sediment thickness of 1.5 km and above were delineated and considered as sub-basins and hence potential areas for hydrocarbon exploration.
- Nwanko, L.I. (2007) Spectral Evaluation of Aeromagnetic Anomaly Map for Geothermal Exploration in Part of Nupe Basin, West Central Nigeria. PhD Thesis, University of Ilorin, Ilorin.
- Reynolds, J.M. (1990) An Introduction to Applied and Environmental Geophysics. John Wiley and Sons Limited, Hoboken, 116-207.
- Abdulsalam, N.N., Nasir, M.A. and Likason, K.O. (2011) Identification of Linear Features Using Continuation Filters over Koton Karfi Area from Aeromagnetic Data. World Rural Observation, 3, 1-8.
- Obaje, G.N., Aduku, M. and Yusuf, L. (2013) The Sokoto Basin of Northwestern Nigeria: A Preliminary Assessment of the Hydrocarbon Prospectivity. Petroleum Technology Development Journal, 3, 66-80.
- Digital Elevation Model (2006) Topographical Map of Latitude 11°30'N-13°30'N and Longitude 4°00'E-6°00'E.
- Kogbe, C.A. (1976) Outline of the Geology of Illummeden Basin, Geology of Nigeria. Elizabethan Publishing Co., 331-338.
- Affodile, M.E. (2002) Ground Water Study and Development in Nigeria. 2nd Edition, Mecon Geology and Eng., Services Ltd., Jos, 453 p.
- Jones, B. (1948) Sedimentary Rocks of the Sokoto Province. Bulletin of the Geological Survey of Nigeria, Vol. 18, Kaduna, 79 p.
- Parker, D.H., Fargher Carter, M.N. and Turner, O.C. (1964) Geological Map of Nigeria Series 1:250,000.
- Bonde, D.S., Udensi, E.E. and Rai, J.K. (2014) Spectral Depth Analysis of Sokoto Basin. Journal of Applied Physics, 6, 15-21.
- Nigerian Geological Survey Agency, NGSA (2006) Geological Map of Latitude 11°30’-13°30’ and Longitude 4°00’ and 6°00’.
- Nigeria Geological Survey Agency, NGSA (2010) High Resolution Aeromagnetic Data, (16 Sheets), Latitude 11°30’-13°30’ and Longitude 4°00’-6°00’.
- Udensi, E.E. (2001) Interpretation of Total Magnetic Field over the Nupe Basin and the Surrounding Basement Complex, Using Aeromagnetic Data. Unpublished PhD Thesis, Ahmadu Bello University, Zaria.
- Oasis montaj 7.0.1 QX Geosoft Inc. Queens Quay Terminal, 207 Queens Quay West Suit 810.
- Parker Gay, S. (1963) Standard Curves for Interpreting Magnetic Anomalies over Long Tabular Bodies. Geophysics, 28, 161-200. https://doi.org/10.1190/1.1439164
- Spector, A. and Grant, F.S. (1970) Statistical Models for Interpreting Aeromagnetic Data. Geophysics, 35, 461-470. https://doi.org/10.1190/1.1440092