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Characteristics, Source Area-weathering, Sedimentary Processes, Tectonic Setting and Taxonomy of Vertisols Developed on Alluvial Sediments in the Benue Trough of North Cameroon

Primus Azinwi Tamfuh, Jean Pierre Temga, Emile Temgoua, Emmanuel Djoufac Woumfo, Philemon Zo'o Zame, Milan Stafford Tchouatcha, Georges Martial Ndzana, Dieudonné Bitom, Veronique Kamgang Kabeyene Beyala

Journal of Geosciences and Geomatics. 2022, 10(1), 1-17 doi:10.12691/jgg-10-1-1
  • Figure 1. Location and Geology of the studied area. (a) Map of Africa locating North Cameroon; (b) Map of North Cameroon locating the Benue Trough; (c) Geological map of the Benue Trough (modified from [21]) and position of pits
  • Figure 2. Morphological view of three Vertisol profiles (P1, P3 and P5) studied in the Benue Basin of North Cameroon
  • Figure 3. X-ray diffraction patterns of Vertisol horizons from Garoua (P1), Bounguel (P3) and Karewa (P5). (S = smectite; = Kaolinite; IL = Illite; IM= Ilmenite; F = Feldspar; G = Goethite; Q = Quartz)
  • Figure 4. X-ray diffraction of the A1 horizon (0-30 cm) from the Benue Basin Vertisols after treatment with ethylene glycol (S= smectite; K= kaolinite; I = Illite)
  • Figure 5. Triangular diagrams of geochemical data. (a) SiO2-Al2O3-Fe2O3 triangular plot of the Vertisols; (b) Al2O3-(CaO*+Na2O)-K2O (A–CN–K) triangular diagram illustrating the degree of chemical weathering in reference to [29]
  • Figure 6. Tectonic setting discrimination diagrams of the Vertisols of the Benue Floodplain. Chart (a) is from [34]; (b) from [35]; (c) from [36] and (d) from [58]. DF1: discrimination function 1; DF2: discrimination function 2 (DF1(Arc-Rift-Collision)=(0.608ln(TiO2/SiO2)(-1.854xln(Al2O3/SiO2) +(0.299ln(Fe2O3/SiO2)+(-0.550ln(MnO/SiO2)+(0.120ln(MgO/SiO2)+(0.194ln(CaO/SiO2)+(-1.510ln(Na2O/SiO2)+(1.94ln(K2O/SiO2)+(0.003ln(P2O5/SiO2) + 0.294; DF2(Arc-Rift-Collision) = (-0.554ln(TiO2/SiO2)+(-0.995ln(Al2O3/SiO2)+(1.765ln(Fe2O3/SiO2) + (-1.391ln(MnO/SiO2) + (-1.034ln(MgO/SiO2) + (0.225ln(CaO/SiO2)+(0.713ln(Na2O/SiO2)+(0.330 ln(K2O/SiO2)+(-0.637ln(P2O5/SiO2)-3.631. A: Oceanic Island; B: Continental Island Arc; C: Active Continental Margin; D: Passive Margin)
  • Figure 7. Proportions of grain shapes in the studied Vertisol samples for different localities in the Benue Basin of North Cameroon
  • Figure 8. Composition and distribution of heavy minerals in the different Vertisol profiles
  • Figure 9. Plot of the studied Vertisols on Herron’s diagram [55]