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2025 | 61 | 2 | 199-214

Article title

Application of high resolution aeromagnetic data for determination of depth to magnetic sources using source parameter imaging in Niger State, Nigeria

Content

Title variants

Languages of publication

EN

Abstracts

EN
Source Parameter Imaging (SPI) is a pivotal geophysical technique, particularly in aeromagnetism, for delineating subsurface geological structures through the analysis of magnetic anomalies. This study applies SPI to high-resolution aeromagnetic data over Baro and its surrounding areas in Niger State, Nigeria, to estimate the depth to magnetic sources. The research emphasizes the characterization of magnetic sources in terms of depth, geometry, dip, and susceptibility contrast. Data processing techniques, including regional field removal, residual anomaly mapping, and reduction to the magnetic equator, were employed to enhance data accuracy and interpretability. The findings reveal significant variations in sedimentary thickness, suggesting potential hydrocarbon reservoirs, particularly in the northern region, characterized by deeper basins. This study underscores the necessity of further exploration, integrating advanced seismic studies and drilling, to assess the hydrocarbon potential accurately. The SPI-derived insights provide a valuable framework for strategic hydrocarbon exploration in Nigeria's interior basins, contributing to the nation's energy security and economic growth.

Year

Volume

61

Issue

2

Pages

199-214

Physical description

Contributors

  • Department of Geology, Faculty of Science, Ekiti State University, Ado Ekiti, Nigeria
  • Physics Department, Federal University of Petroleum Resources Effurun, Delta State, Nigeria
  • Department of Petroleum Engineering and Geosciences, Petroleum Training Institute, Effurun, Nigeria
  • Department of Geology, Faculty of Science, Dennis Osadebay University, Asaba, Delta State, Nigeria
  • Department of Physics, Faculty of Science, Dennis Osadebay University, Asaba, Delta State, Nigeria

References

  • [1] Alalade, B., and Tyson, R.V. (2013). Influence of igneous intrusions on thermal maturity of Late Cretaceous shales in the Tuma well, Chad Basin, NE Nigeria. Journal of African Earth Sciences, 77, 59-66. https://doi.org/10.1016/j.jafrearsci.2012.09.006
  • [2] Alhassan, U., Obiora, D., and Okeke, F. (1970). The assessment of aquifer potentials and aquifer vulnerability of southern Paiko, north central Nigeria, using geoelectric method. Global Journal of Pure and Applied Sciences, 21(1), 51-70
  • [3] Bird, D.E. (1997). Primer. Interpreting Magnetic data. America Association of Petroleum Geologist Explorer 18(5), 18-21
  • [4] Blakely, R.J., and Simpson, R.W. (1986). Approximating edges of source bodies from magnetic or gravity anomalies. Geophysics, 51(7), 1341-1519. https://doi.org/10.1190/1.1442197
  • [5] Clark, A.J. (1996). Seeing Beneath the Soil: Prospecting Methods in Archaeology. B.T. Batsford Ltd.
  • [6] Dietze, F., Kontny, A., Heyde, I., and Vahle, C. (2008). Rock magnetic properties of basalt lithologies and subsurface modeling from magnetic field data for the Reykjanes peninsula (Iceland). Geotectonic Research, 95, 33-35. https://doi.org/10.1127/1864-5658/08/9501-0033
  • [7] Dobrin, M., and Savit, C. (1988).Introduction to Geophysical Prospecting (Fourth Editioned.). Singapore: McGraw-Hill.
  • [8] Flanagan, G., and Bain, J. (2013). Improvements in magnetic depth estimation: application of depth and width extent nomographs to standard depth estimation techniques. First Break, 31(12). https://doi.org/10.3997/1365-2397.2013028
  • [9] Goodge, J.W. (2020). Geological and tectonic evolution of the Transantarctic Mountains, from ancient cratonto recent enigma. Gondwana Research, 80, 50-122. https://doi.org/10.1016/j.gr.2019.11.001
  • [10] Gordienko, V. (2019).Earth crust in oceans and strip anomalies of magnetic field. Geology and Mineral Resources of World Ocean, 15(4), 3-35. https://doi.org/10.15407/gpimo2019.04.003
  • [11] Hinze, W.J., Von Frese, R.R.B., Von Frese, R., and Saad, A.H. (2013).Gravity and Magnetic Exploration. Cambridge University Press.
  • [12] Hutchens, M. (2018). Depth Estimation of Source Bodies Using 2D Magnetic Gradient Ratios. ASEG Extended Abstracts, 2018(1), 1-1. https://doi.org/10.1071/aseg2018abp081
  • [13] Jezierska, A., Luczyński, P., and Staśkiewicz, A. (2016). Carbonate-clastic sediments of the Dudziniec Formation in the Kościeliska Valley (High-Tatric series, Tatra Mountains, Poland): role of syndepositional tectonic activity in facies development during the Early and Middle Jurassic. Geological Quarterly 60 (4): 869-880. http://dx.doi.org/10.7306/gq.1327
  • [14] Johnson, W.W. (1969). A least - Squares method of interpreting magnetic anomalies caused by Two- Dimensional structures. Geophysics, 34, 65-74
  • [15] Krzaklewski, P. (2012). Formation and role of neogene sediments from Tatra Mountains in the shaping of CzarnaOrawa river alluvial plain. Quaestiones Geographicae, 31(3), 41-46. https://doi.org/10.2478/v10117-012-0003-y
  • [16] Mamman, E. (2021). Resolving the Farmers- Herders Conflict in Nigeria: A Way Forward for Sustainable National Development. International Journal of Social Science and Human Research, 04(07). https://doi.org/10.47191/ijsshr/v4-i7-19
  • [17] Mandea, M., and Korte, M. (2010). Geomagnetic Observations and Models. Springer Dordrecht. https://doi.org/10.1007/978-90-481-9858-0
  • [18] Nabighian, M.N. (1972). The Analytic Signal of Two-Dimensional Magnetic Bodies with Polygonal Cross-section: Its Properties and Use for Automated Anomaly Interpretation. Geophysics, 37(3), 507-517
  • [19] Nigerian Geological Survey Agency Abuja.(2009). High Resolution Airborne Geophysical Series- Magnometer Survey Grid Map of Total Intensity (1 sheet). Scale 1: 100,000.
  • [20] Opara A.I., Udoete R.L., Emberga T.T., Echetama H.N., Ugwuegbu I.E., Nwokocha K.C., Ijeoma K.C., Chinaka J.C., and Onyema J.C. (2015). Structural Interpretation of the Jos-Bukuru Younger Granite Ring Complexes Inferred from Landsat-TM Data. Journal of Geosciences and Geomatics 3(3), 56-67 doi:10.12691/jgg-3-3-2
  • [21] Sawuta, J.M.; Ayanninuola O.S, Udensi E.E, Ogwola P. (2019). Estimation Of Magnetic Depth To Source Using High Resolution Of Aeromagnetic Data Of Parts Of Upper Benue Trough, North Eastern Nigeria. Science World Journal 14(1), 7-11
  • [22] Schillawski, S., and Petsch, S. (2008). Release of biodegradable dissolved organic matter from ancient sedimentary rocks. Global Biogeochemical Cycles, 22(3), GB3002. https://doi.org/10.1029/2007gb002980
  • [23] Siart, C., Forbriger, M., Bubenzer, O. (2018). Digital Geoarchaeology: Bridging the Gap Between Archaeology, Geosciences and Computer Sciences. In: Siart, C., Forbriger, M., Bubenzer, O. (eds) Digital Geoarchaeology. Natural Science in Archaeology. Springer, Cham. https://doi.org/10.1007/978-3-319-25316-9_1
  • [24] Skeels, D.C. (1967). What is Residual Gravity? Geophysics, 32, 872-876
  • [25] Smith, R.S., and Salem, A. (2005). Imaging depth, structure, and susceptibility from magnetic data: The advanced source-parameter imaging method. Geophysics 70(4), L31–L38. https://doi.org/10.1190/1.1990219
  • [26] Smith, R.S., Thurston, J.B., Dai, T., and MacLeod, L.N. (1998). The Improved Source Parameter Imaging Method. Geophysical Prospecting, 46, 141-151
  • [27] Thompson, D.T., Ritter, O., and Cordell, L. (2017). Euler Deconvolution: A Tool for Tectonic Interpretation and Paleomagnetic Analysis of Magnetic Data. In Geophysical Case Study of the Woodlawn Orebody, N.S.W., Australia (pp. 55-60). Springer, Cham.
  • [28] Thurston, J.B., and Smith, R.S. (1997). Automatic Conversion of Magnetic Data to Depth, Dip, and Susceptibility Contrast using the SPI Method. Geophysics Vol. 62, No. 33, 807-813. https://doi.org/10.1190/1.1444190

Document Type

article

Publication order reference

Identifiers

YADDA identifier

bwmeta1.element.psjd-4a037ec2-c94b-4a11-9617-d57b368e2c4d
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