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Abstrakty
We present the detail basement and trends of geological structures associated with the Mesozoic-Cenozoic volcanism in the south–western region of the Nigerian Benue trough using recent gravity and magnetic anomalies of the region. The analysis aimed at recognizing and mapping the basement structure that controlled the distribution and source host of hydrocarbon and other economic mineral resources in the region. The structural recognition and mapping is done on the basis of the utilization of the Tilt Angle (TA) and Total Horizontal Derivative of the Tilt Angle (THDTA) of gravity and magnetic data. From these techniques, we have been able to identify and mapped out those edges of anomalous sources due to the gravity and magnetic data that are in association with the basement geological structures of the area. Based on the mapped structural trends, it is observed that the basement structures derived from both the gravity and magnetic anomalies correlated well with the zones of volcanic rocks around Gboko and area between Lefin and Oturkpo. The two locations are sitting over gravity and magnetic highs suggesting high density and susceptibility material below the subsurface. The Euler deconvolution method suggested depths between 1 and 5 km from both gravity and magnetic data. Deeper basement of anomalous sources are suggested between 3 and 5 km. The 1 km depth interprets the regions of basement highs or corresponding to intrusive zones.
Wydawca
Czasopismo
Rocznik
Tom
Strony
1595--1606
Opis fizyczny
Bibliogr. 45 poz., rys., tab.
Twórcy
autor
- Physics Unit, Department of Science Laboratory Technology, Modibbo Adama University, Yola P.M.B. 2076, Nigeria
autor
- CSIR-National Institute of Oceanography, Dona Paula, Goa 403004, India
autor
- Physics Unit, Department of Science Laboratory Technology, Modibbo Adama University, Yola P.M.B. 2076, Nigeria
autor
- Department of Applied Geophysics, Indian Institute of Technology (Indian School of Mines), Dhanbad 826004, India
autor
- Nigerian Geological Survey Agency (NGSA), Abuja Office, Abuja, Nigeria
Bibliografia
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- 2. Abdelrahman EM, El-Araby TM, Essa KS (2003b) Shape and depth solutions from third moving average residual gravity anomalies using the window curves method. Kuwait J Sci Eng 30:95–108
- 3. Abdelrahman EM, El-Araby TM, Essa KS (2003c) A least-squares minimisation approach to depth, index parameter, and amplitudę coefficient determination from magnetic anomalies due to thin dykes. Explor Geophys 34:241–248
- 4. Abdelrahman EM, Abo-Ezz ER, Essa KS, El-Araby TM, Soliman KS (2007) A new least-squares minimization approach to depth and shape determination from magnetic data. Geophys Prospect 55:433–446
- 5. Abdullahi M, Kumar R (2020) Curie depth estimated from high-resolution aeromagnetic data of parts of lower and middle Benue trough (Nigeria). Acta Geod Geoph 55(4):627–643
- 6. Abdullahi M, Kumar R (2021) Basement and structure near the south-western margin of the lower Benue trough between, and including, the Anambra Basin and Afikpo Syncline, as derived from aeromagnetic and gravity data. Pure Appl Geophys. https://doi.org/10.1007/s00024-021-02801-3
- 7. Abdullahi M, Singh UK (2018) Basement geology derived from gravity anomalies beneath the Benue trough of Nigeria. Arab J Geosci 11:694
- 8. Abdullahi M, Singh UK, Roshan R (2019a) Mapping magnetic lineaments and subsurface basement beneath parts of lower Benue trough (LBT), Nigeria: insights from integrating gravity, magnetic and geologic data. J Earth Syst Sci 128:17
- 9. Abdullahi M, Kumar R, Singh UK (2019b) Magnetic basement depth from high-resolution aeromagnetic data of parts of lower and middle Benue trough (Nigeria) using scaling spectral method. J Afr Earth Sci 150:337–345
- 10. Abdullahi M, Singh UK, Modibbo UM (2019c) Crustal structure of southern Benue trough, Nigeria from 3D inversion of gravity data. J Geol Min Res 11(4):39–47
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Uwagi
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2024).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-32c6b868-4dff-4aaa-a6d4-44b700c9bfd9