Re-Evaluation of Hydrocarbon Potentials of Eastern Part of the Chad Basin, Nigeria: An Aeromagnetic Approach*
Emmanuel Kenechukwu Anakwuba, Augustine Ifeanyi Chinwuko
Abstract
Emmanuel Kenechukwu Anakwuba, Augustine Ifeanyi Chinwuko
Abstract
The hydrocarbon potentials of parts of the Nigerian sector of the Chad Basin have been re-evaluated from the interpretation of aeromagnetic anomalies. Nine aeromagnetic maps located between latitudes 11 o 00 min - 12 o 30 min N and longitudes 12 o 30 min - 14 o 00 min E were assembled and analyzed to determine the structural pattern and the sedimentary thickness variations within the basin. The qualitative interpretation indicates that the area is intensely fractured with major faults trending in a NE-SW direction. The aeromagnetic data were subjected to Fourier analysis and results show two depth sources in the study area; the shallower sources have a average value of 1.8 km while the deeper ones have an average value of 4.3 km. The sedimentary thickness of the area ranges from 1.0 to 5.8 km. Based on the computed sedimentary thicknesses and the temperature at depth (125-228 o C), some parts of the study area have been demarcated for detail hydrocarbon exploration.
OpenAlex reports 7 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
The hydrocarbon potentials of parts of the Nigerian sector of the Chad Basin have been re-evaluated from the interpretation of aeromagnetic anomalies. Nine aeromagnetic maps located between latitudes 11 o 00 min - 12 o 30 min N and longitudes 12 o 30 min - 14 o 00 min E were assembled and analyzed to determine the structural pattern and the sedimentary thickness variations within the basin. The qualitative interpretation indicates that the area is intensely fractured with major faults trending in a NE-SW direction. The aeromagnetic data were subjected to Fourier analysis and results show two depth sources in the study area; the shallower sources have a average value of 1.8 km while the deeper ones have an average value of 4.3 km. The sedimentary thickness of the area ranges from 1.0 to 5.8 km. Based on the computed sedimentary thicknesses and the temperature at depth (125-228 o C), some parts of the study area have been demarcated for detail hydrocarbon exploration.
Key concepts: Geology, Structural basin, Sedimentary rock, Sedimentary basin, Latitude, Hydrocarbon exploration, Hydrocarbon, Geomorphology