Figures index

From

Lithofacies Characterization of Sedimentary Succession from Oligocene to Early Miocene Age in X2 Well, Greater Ughelli Depo Belt, Niger Delta, Nigeria

Lucas F.A, Omodolor Hope E

Journal of Geosciences and Geomatics. 2018, 6(2), 77-84 doi:10.12691/jgg-6-2-5
  • Figure 1. Map showing the distribution of Depo Belts within the Niger Delta and the location of the study area within the Greater Ughelli Depo belt [9]
  • Figure 2. Lithostratigraphy analysis of samples from X2 Well, Greater Ughelli Depo-Belt (6.09m-4817m)
  • Figure 3. Lithostratigraphy analysis of samples from X2 Well, Greater Ughelli Depo-Belt (500m-1067.1m)
  • Figure 4. Lithostratigraphy analysis of samples from X2 Well, Greater Ughelli Depo-Belt(1065.4m-1628m)
  • Figure 5. Lithostratigraphy analysis of samples from X2 Well, Greater Ughelli Depo-Belt(1969.5m-2268.3m)
  • Figure 6. Lithostratigraphy analysis of samples from X2 Well, Greater Ughelli Depo-Belt(2286.6m-2567.1m).
  • Figure 7. Lithostratigraphy analysis of samples from X2 Well, Greater Ughelli Depo-Belt (2585.4m-2932.9m)
  • Figure 8. Lithostratigraphy analysis of samples from X2 Well, Greater Ughelli Depo-Belt(6.09m-3603.7m).
  • Figure 9. Lithostratigraphy analysis of samples from X2 Well, Greater Ughelli Depo-Belt (29512m-3384.2m)
  • Figure 10. Lithostratigraphy analysis of samples from X2 Well, Greater Ughelli Depo-Belt (3384.2m-3603.7m)
  • Figure 11. Proposed paleodepositional model for the deposition of X2 well sediment in the shelfal environment