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Structural features derived from a multi-method approach and 2.75D modelling of aeromagnetic data: a case study of the Pitoa–Figuil area (Northern Cameroon)

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
An interpretation of aeromagnetic data was conducted in the Pitoa–Figuil area (Northern Cameroon). The aim of this investigation was the first to emphasise lineaments hidden under geological formations and secondly to propose two 2.75D models of the subsurface structures. Different magnetic data processing techniques were used, notably horizontal gradient magnitude, analytic signal and Euler deconvolution. The application of these techniques made it possible to map a certain number of lineaments representing discontinuities of magnetic susceptibility, mainly oriented NE–SW, NW–SE, E–W and ENE–WSW. The predominant direction for major lineaments is NE–SW and NW–SE. The major NE–SW trends have been attributed to the consequences of the Benue trough set-up due to the Atlantic opening. The lineaments map associated with the Euler solutions permits us to highlight and characterise 18 faults and some intrusive bodies. Euler solutions indicate depths down to 5.3 km for anomaly sources. The 2.75D modelling from the aeromagnetic anomaly reduced to the equator permits to understand the stratification of the deep and near-surface structures, which are sources of the observed anomalies. The sediment thickness values (3.5–4 km) combined with the presence of numerous deep faults make this area a potential site for hydrocarbon accumulations.
Czasopismo
Rocznik
Strony
587--600
Opis fizyczny
Bibliogr. 34 poz.
Twórcy
  • Postgraduate School of Science, Technology and Geosciences, University of Yaoundé I, P.O. Box 47, Yaoundé, Cameroon
  • Postgraduate School of Science, Technology and Geosciences, University of Yaoundé I, P.O. Box 47, Yaoundé, Cameroon
  • Department of Physics, Advanced Teacher’s Training College, University of Yaoundé I, P.O. Box 47, Yaoundé, Cameroon
autor
  • School of Geology and Mining Engineering, University of Ngaoundéré, P.O. Box 115, Meiganga, Cameroon
  • Postgraduate School of Science, Technology and Geosciences, University of Yaoundé I, P.O. Box 47, Yaoundé, Cameroon
  • Postgraduate School of Science, Technology and Geosciences, University of Yaoundé I, P.O. Box 47, Yaoundé, Cameroon
Bibliografia
  • 1. Achilleos GA (2010) Approaching a model for estimating horizontal errors of digitized contours. J Spat Sci 55:147–164. https://doi.org/10.1080/14498596.2010.487856
  • 2. Akande SO, Egenhoff SO, Obaje NG, Ojo OJ, Adekeye OA, Erdtmann BD (2012) Hydrocarbon potential of cretaceous sediments in the lower and middle benue trough, nigeria: insights from new source rock facies evaluation. J Afr Earth Sci 64:34–47
  • 3. Blakely RJ, Simpson RW (1986) Approximating edges of source bodies from magnetic or gravity anomalies. Geophysics 51:1494–1498
  • 4. Clark DA, Emerson DW (1991) Notes on rock magnetization characteristics in applied geophysical studies. Explor Geophys 22:547–555
  • 5. Daouda D, Tchameni R, Bascou J, Wangmene SA, Tchunte PM, Bouchez JL (2017) Microstructures and magnetic fabrics of the ngaoundéré granite pluton (Cameroon): Implications to the late-pan-african evolution of central cameroon shear zone. J Afr Earth Sci 129:887–897
  • 6. Durrheim RJ, Cooper RJ (1998) EULDEP: a program for the euler deconvolution of magnetic and gravity data. Comput Geosci 6:545–550
  • 7. Grauch VJ, Cordell L (1987) Limitations of determining density or magnetic boundaries from the horizontal gradient of gravity or pseudogravity. Geophysics 52:118–121
  • 8. Houketchang BM, Penaye J, Njel UO, Moussango AP, Sep JP, Nyama BA, Wassouo WJ, Abate JM, Yaya F, Mahamat A, Hao Y, Fei Y (2016) Geochronological, geochemical and mineralogical constraints of emplacement depth of TTG suite from the sinassi batholith in the Central African fold belt (CAFB) of northern Cameroon: implications for tectonomagmatic evolution. J Afr Earth Sc 116:9–41
  • 9. Jeng Y, Lee YL, Chen CY, Lin JM (2003) Integrated signal enhancements in magnetic investigation in archaeology. J Appl Geophys 53:31–48
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  • 11. Kamguia J, Manguelle-Dicoum E, Tabod CT, Tadjou JM (2005) Geological models deduced from gravity data in the Garoua basin, Cameroon. J Geophys Eng 2:147–152
  • 12. Keating P, Pilkington M (2004) Euler deconvolution of the analytic signal and its application to magnetic interpretation. Geophys Prospect 52(3):165–182
  • 13. Khattach D, Mraoui H, Sbibih D, Chennouf T (2006) Analyse multi-échelle par ondelettes des contacts géologiques: application à la vimétrique du maroc nord oriental. Geoscience 338:521–526
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  • 17. Ngako V, Affaton P, Nnange JM, Njanko T (2003) Pan-African tectonic evolution in central and Southern Cameroon: transpression and transtension during sinistral shear movements. J Afr Earth Sci 36:207–214. https://doi.org/10.1016/S0899-5362(03)00023-X
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  • 23. Ntsama AJ, Bessong M, Hellc JV, Mbesse CO, Nolla JD, Dissombo EA, Takem EJ, Mbassa BJ, Mouloud B, Vignaud PJ, Mfoumbeng MP (2014) The importance of diagenetic processes in sandstones facies of the hamakoussou sedimentary basin in North Cameroon: influence on reservoir quality. Int J Sci Basic Appl Res 13:220–230
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Uwagi
Opracowanie rekordu ze środków MNiSW, 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-67859483-7831-45bf-9c0e-ff361a1b06d0
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