Aeromagnetic Evaluation of Structural Features and Depth to Basement at the Basement-Dahomey Basin Transition Zone, Abeokuta and Environs, Southwestern Nigeria
Keywords:
Abeokuta, Dahomey Basin, Lineament, Euler Deconvolution, AeromagneticAbstract
This study was aimed at evaluating a contact zone and structural framework between the Basement Complex and the Dahomey Basin of Southwestern Nigeria. Qualitative and quantitative analyses were used to delineate the geologic structures as well as the sedimentary thickness of 55m to 575m by measurement of depth to magnetic sources. The qualitative analysis on the total magnetic intensity (TMI) data was attained by applying different filters which include reduction to the magnetic equator (RTE), tilt angle derivative (TDR), analytical signal and lineaments extraction to enhance magnetic anomalies. The quantitative analysis which includes Source Parameter Imaging (SPI) and 3D-Euler deconvolution (ED) aided the assessment of structural depth to magnetic sources. The qualitative interpretation revealed the distribution of magnetically susceptible anomalies with varying intensities across the study area. The TMI showed rightly positioned magnetic intensity range of 33,028nT to 33,087nT revealing areas of high and low magnetic intensity. The TDR ranged between -1.4nT to 1.4nT while the Analytic signal ranged between 117nT/m and 8615 nT/m with magnetic peaks in the northeast, west and southwest parts of the study area; interpreted as faulted basement blocks with delineated fault-zones trending northeast. The SPI was used in determining depth to basement and with a range of 54.1m to 599.1m. The 3D-ED ranged between -251.7m to 575.4m with observed anomaly trending in direction of NE-SW implying its conformity to Pan-African Orogeny. The Interpretation of structural features is highly significant for entrapment which can aid accumulation of valuable mineralization and localization of competent areas for proposed engineering construction.
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