Tytuł artykułu
Wybrane pełne teksty z tego czasopisma
Identyfikatory
Warianty tytułu
Języki publikacji
Abstrakty
The aim of this study is to improve the structural map of Douala-Kribi basin. For this purpose, computer tools are used to make qualitative and quantitative analyses to interpret the gravity data. The findings provided several maps which are: the Bouguer gravity anomalies, residual, horizontal gradient, analytical signal, tilt angle, variation of depth, and multi-scale analysis gravity anomalies maps. A thorough examination of these maps highlights lineaments interpreted as faults, and intrusive bodies in the study area. The multi-scale analysis helped to portray the deep faults and therefore construct the structural map of the Douala-Kribi basin. The application of the Euler deconvolution method and variation of the maxima solutions of horizontal gradient upward continuation (HGup) have resulted in the depth of the structures and the intrusive bodies. The faults identified in the Douala-Kribi basin seem to be induced by tectonic movements in addition to the uprise of intrusion. The Euler solutions and tilt angle depths are included in those of the residual field while those from the analytical signal partly overlap those from the residual field and tilt angle. Then, the Euler solutions maps, and the maxima solutions contribute to highlighting the trust interval depth which is the compatibility depth.
Wydawca
Czasopismo
Rocznik
Tom
Strony
49--65
Opis fizyczny
Bibliogr. 57 poz.
Twórcy
autor
- 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
autor
- Department of Physics, Advanced Teacher’s Training College, University of Yaoundé I, P.O. Box 47, Yaoundé, Cameroon
Bibliografia
- 1. Amar M, Manar A, Boualoul M (2012) Apport de la cartographie aéromagnétique a Identification structurale du Systeme aquifere des sources de l’Oasis de Figuig (Maroc). Bulletin De L’institut Scientifique, Rabat, Section Sciences De La Terre 34:29-40
- 2. Blakely RJ, Simpson RW (1986) Approximating edges of source bodies from magnetic or gravity anomalies. Geophysics 51:1494-1498
- 3. Bouiflane M (2008) Cartographie aéromagnétique et magnétique mul-tiéchelles: Etude structurale d’une région du Fossé Rhénan. These de Doctorat de Géophysique, Université Louis Pasteur-Strasbourg I. 206 pages
- 4. Boukeke DB (1994) Structures crustales d’Afrique centrale déduite des anomalies gravimétriques et magnétiques: le domaine pré-cambrien de la République Centrafricaine et du Sud-Cameroun. These de Doctorat, université de Paris Sud, p. 264
- 5. Burger H, Sheehan AF, Craig HJ (2006) Introduction to applied geophysics (Exploring the shallow subsurface). W.W. Norton & Company, New York
- 6. Cheunteu Fantah CA, Adiang Mezoue C, Mouzong MP, Tokam Kamga AP, Nouayou R, Nguiya S (2022) Mapping of major tectonic lineaments across Cameroon using potential field data. Earth Planets Space 74:59. https://doi.org/10.1186/s40623-022-01612-7
- 7. Cordell L, Grauch VJS (1985) Mapping basement magnetization zones from aeromagnetic data in the San Juan basin, New Mexico. In: Hinze WJ (ed) The utility of regional gravity and magnetic anomaly maps. Society of Exploration Geophysicists, Houston
- 8. Dumont JF (1986) Identification par Télédétection de L’accident de la Sanaga (Cameroun). Sa Position dans le Contexte des Grands Accidents de l’Afrique Centrale et de la Limite nord du Craton Congolais. Géodynamique 1:13-19
- 9. Feumoe ANS, Ndougsa-Mbarga T, Manguelle-Dicoum E, Derek Fairhead J (2012) Delineation of tectonic lineaments using aeromagnetic data for the southeast Cameroon area. Geofizika 29(2):175-192
- 10. Kennedy WQ (1964) The structural differentiation of Africa in the Pan-African (500 m). Tectonic episode. 8th Ann. Rep. Res.Inst. African geol. Univ. Leeds. p 48
- 11. Khattach D, Keating P, Mili EM, Chennouf T, Andrieux P, Milhi A (2004) Apport de gravimétrie a l’étude de la structure du basffa (Maroc nordoriental): implications hydrogéologiques. Géoscience 336:1427-1432
- 12. Khattach D, Mraoui HD, Sbibih T, Chennouf Q (2006) Analyse multi-échelle par ondelettes des contacts géologiques : application a la gravimétrique du Maroc nord-oriental. C. R. Géosci 338:521-526
- 13. Koumetio F (2004) Contribution géophysique par méthode gravimét-rique a l’étude des structures profondes de la marge occidentale du Craton du Congo dans la région de Kribi (Cameroun). These de Doctorat 3e cycle. Université de Yaoundé I. p 110
- 14. Kue Petou RM, Owona Angue MLC, Njingti Nfor N, Manguelle-Dicoum E (2017) 3D modelling from new and existing gravity data of an intrusive body in the northern part of Kribi-Campo sub basin in Cameroon. Int J Geosci 8:984-1003. https://doi.org/10. 4236/ijg.2017.88056
- 15. Kue Petou RM, Owona Angue MLC, Njingti N, Eloundou EL, Mioumnde AP, Kue Negham MC, Manguelle-Dicoum E, Weiqi S (2020) Interprétation quantitative des anomalies gravimétriques
- 16. dans le bassin de Kribi - Campo (Sud - Cameroun) basée sur l’analyse spectrale et la modélisation 2.5 : implications struc-turales. J Int Géosci. Vol. 9, No. 3
- 17. Lowrie W (1997) Fundamentals of geophysics, Second Edition, Swiss Federal Institute of Technology. Cambridge Universty Press, Zürich, p 2013
- 18. Marson I, Klingele EE (1993) Advantages of using the vertical gradient of gravity for 3-D interpretation. Geophysics 58:1588-1595
- 19. Miller HG, Singh V (1994) Potential field tilt- a new concept for location of potential field sources. J Appl Geophys 32:213-217
- 20. Minyem D, Nedelec A (1990) Origin and evolution of the Eseka Gneisses (Cameroon). Archean TTG reworked in the Panafrican mobile belt. In: Proceedings of the 15th Colloquium of African Geology, Nancy. Vol. 2. pp 21-24
- 21. Muzaffer Ö, Ünal D (2013) Edge detection of magnetic sources using enhanced total horizontal derivative of the tilt angle. Bull Earth Sci Appl Res Centre Hacettepe Univ Yerbilimleri 34(1):73-82
- 22. Nabighian MN (1972) The analytic signal of two-dimensional magnetic bodies with polygonal cross-section: its properties and use for automated anomaly interpretation. Geophysics 37:507-517
- 23. Nabighian MN (1974) Additional comments on the analytic signal of two dimensional magnetic bodies with polygonal cross-section. Geophysics 39:85-92
- 24. Nabighian MN (1984) Toward a three-dimensional automatic interpretation of potential field data via generalized Hilbert transforms: fundamental relations. Geophysics 49:780-786
- 25. Ndikum EN, Tabod CT (2023) Regional intrusive signature from the Cameroon coastal basins to Bioko Island in equatorial Guinea (Gulf of Guinea) using gravity studies. J Geosci Environ Prot 1(1):1-14. https://doi.org/10.4236/gep.2023.111001
- 26. Ndougsa Mbarga T, Feumoe AN, Manguelle-Dicoum E, Derek Fairhead J (2012) Aeromagnetic data interpretation to locate buried faults in South-East Cameroon. Geophysica 48:49-63
- 27. 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 Sc 36:207-214. https://doi.org/10.1016/S0899-5362(03)00023-X
- 28. Noutchogwe C, Tabod C, Manguelle-Dicoum E (2006) A gravity study of the crust beneath the Adamawa Fault Zone, West Central Africa. J Geophys Eng 3:82-89. https://doi.org/10.1088/17422 132/3/1/009
- 29. Ntepe N, Aka FT, Ubangoh RU, Ateba B, Nnange JM, Hell JV (2004) The July 2002 earthquake in the Kribi region: geological context and a preliminary evaluation of seismic risk in southwestern Cameroon. J Afr Earth Sc 40:163-172
- 30. Nzenti JP, Barbey P, Macaudiere J, Soba D (1988) Origin and evolution of the late Precambrian high-grade Yaoundé gneisses (Cameroon). Precambrian Res 38:91-109
- 31. Nzenti JP, Barbey P, Bertrand JML, Macaudiere J (1994) La chaíne panafricaine au Cameroun: cherchons suture et modele. In : S.G.F. édit., 15e réunion des Sciences de la Terre, Nancy, France. p 99
- 32. Owona Angue MLC, Nguiya S, Nouayou R, Tokam Kamga AP, Manguelle-Dicoum E (2011) Geophysical investigation of the transition zone between the Congo Craton and the Kribi-Campo Sedimentary basin (South-west Cameroon). S Afr J Geol 114(2):145-158. https://doi.org/10.2113/gssajg.114.2.145
- 33. Owona Angue MLC, Assembe SP, Nfor N, Ngoh JD, Ndougsa MT, Kue Petou R, Bisso D (2016) Determination of the structural lineaments in the Kribi-Campo-Ma’an area from a multi-scale analysis of gravity data using the HGM and Euler 3D deconvolution approaches. Int J Geosci 7:1122-1143. https://doi.org/10.4236/ ijg.2016.79085
- 34. Owono Angue MLC (2012) Investigation Géophysique de la zone de transition entre le bassin sédimentaire de Kribi-Campo et la bor-dure Nord-Ouest du Craton du Congo. These de Doctorat/PhD, Univesité de Yaonudé I
- 35. Perez-Diaz L, Eagles G (2014) Constraining South Atlantic growth with seafloor spreading data. Tectonics 33:1848-1873. https:// doi.org/10.1002/2014TC003644
- 36. Phillips JD (1998) Processing and interpretation of aeromagnetic data for the Santa Cruz Basin—Patahonia Mountains Area, SouthCentral Arizona. U.S. Geological Survey Open File Report, Arizona, 02-98.
- 37. Reid AB, Fitzgerald DJ (2005) Estimation de la profondeur du sous-sol magnetique d’Euler hybride: tests 3D de Bishop. Dans SEG Tech Progr Expended Abstr. https://doi.org/10.1190/1.2144412
- 38. Reid AB, Allsop JM, Granser H, Millet AJ, Somerton IW (1990) Magnetic interpretation in three dimensions using Euler deconvolution. Geophysics 55(1):80-91. https://doi.org/10.1190/1.1442774
- 39. Rocci G (1965) Essai d’interprétation de mesures géochronologiques. La structure de L’ouest Africain. Coll Intem Géochronol Nancy Sci Terre 10:461-478
- 40. Roest WR, Verhoef J, Pilkington M (1992) Magnetic interpretation using the 3-D analytic signal. Geophysics 57(1):116-125
- 41. Salem A, William S, Fairhead D, Smith R, Ravat D (2008) Interpretation of magnetic data using tilt angle derivatives. Geophysics 73:1-10
- 42. Shandini Y, Tadjou JM (2012) Interpretation gravity anomalies in south Cameroon. Central Earth Sci Res J 16:5-9
- 43. Shandini NY, Tadjou JM, Tabord CT, Fairheard JD (2010) Gravity data interpretation in the northern edge of the Congo Craton, South-Cameroon. Anuario Do Instituto De Geociěncias 33:73-82
- 44. Tadjou JM, Nouayou R, Kamguia J, Kande HL, Manguelle-Dicoum E (2009) Gravity analysis of the boundary between the Congo craton and the pan-African belt of Cameroon. Austr J Earth Sci 102:71-79
- 45. Tchameni R, Mezger K, Nsifa N, Pouclet A (2001) Crustal origin of early Proterozoic syenites in the Congo Craton (Ntem complex), south Cameroon. Lithos 57:23-42
- 46. Tchameni R, Pouclet A, Penaye J, Ganwa AA, Toteu SF (2006) Petrography and geochemistry of the Ngaoundéré Pan-African granitoids in Central North Cameroon: implications for their sources and geological setting. J Afr Earth Sci 44(4-5):511-529. https://doi. org/10.1016/j.jafrearsci.2005.11.017
- 47. Thompson DT (1982) EUlDPH: a new technique for making computer-assisted depth estimates from magnetic data. Geophysics 47:31-37. https://doi.org/10.1190/1.1441278
- 48. Tokam KAP, Tabod CT, Nyblade AA, Julia J, Wiens DA, Pasyanos M (2010) Structure of the crust beneath Cameroon, West Africa, from the joint inversion of Rayleigh wave group velocities and receiver functions. Geophys J Int 183:1061-1076. https://doi.org/ 10.1111/j.1365-246X.2010.04776.x
- 49. Toteu SF, Van Schmus RW, Penaye J, Nyobe JB (1994) U-Pb and Sm-Nd evidence for Eburnian and pan-African high-grade metamorphism in cratonic rocks of southern Cameroon. Precambr Res 67:321-347
- 50. Toteu SF, Penaye J, Poudjoum Djomani Y (2004) Geodynamic evolution of the pan-African belt in Central Africa with special reference to Cameroon. Can J Earth Sci 41:73-85. https://doi.org/10. 1139/e03-079
- 51. Toteu SF, Penaye J, Deschamps Y, Maldan F, Myama Atibagoua B, Bouyo Houketchang M, Sep Nlomgan JP, Mbola Dzana SP (2008) Géologie et ressources minerales du Cameroun, 33rd international geological congress, Oslo, Norway, 6-14 August
- 52. Vanié LTA, Khattach D, Houari MR (2005) Apport des filtrages des anomalies gravimétriques a l’étude des structures profondes du Maroc oriental. Bulletin Institut Des Sciences De Rabat, Section Sciences De La Terre 27:29-40
- 53. Verduzco B, Fairhead JD, Green CM, Mackenzie C (2004) New insights into magnetic derivatives for structural mapping. Lead Edge 23:116-119
- 54. Vicat JP, Bilong P (1998) Esquisse géologique du Cameroun. Collection GEOCAM. Presses Universitaires De Yaoundé I:3-11
- 55. Yandjimain J, Ndougsa-Mbarga T, Meying A, Bi-Alou MB, Ngou-mou PC, Assembe SP, Ngoh JD, Owono-Amougou OUI (2017) Combination of tilt-angle and euler deconvolution approaches to determine structural features from aeromagnetic data modeling over Akonolinga-Loum area (CentreEast, Cameroon). Int J Geosci 8:925-947. https://doi.org/10.4236/ijg.2017.87053
- 56. Yandjimain J, Ndougsa-Mbarga T, Bi-Alou MB, Meying A (2018) Aeromagnetic data modeling for geological and structural mappings over the DJADOM-ETA area, in the Southeastern Cameroon. Int J Geosci 9:354-370. https://doi.org/10.4236/ijg.2018.96022
- 57. Yandjimain J, Ndougsa-Mbarga T, Meying A, Ngoumou PC (2020) Evidences by multiscale analysis and 2D3/4 models from the magnetic anomalies and iron mineralization (BIF) over the DJADOM-ETA area, Southeastern Cameroon. Open J Earthq Res 9:19-32. https://doi.org/10.4236/ojer.2020.91002
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-32865f43-6864-4c1c-a95d-69265c6cb720