Preliminary results from a pseudogravity study of the Benue Trough, Nigeria

Charles O. Ofoegbu
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引用次数: 8

Abstract

As part of a Benue Trough project, a pseudogravimetric study of the Benue Trough is being carried out and preliminary results of this study are here presented. Several aeromagnetic profiles have been taken across the Benue Trough and transformed to their corresponding pseudogravimetric profiles using the equivalent layer method. Qualitative interpretation and comparison of the pseudogravimetric, aeromagnetic and gravity profiles have been carried out in order to find possible origins of the short and long wavelength anomalies observed over the trough. The results of this analysis point to the fact that the short wavelength anomalies are possibly due to the minor intrusive bodies at shallow depths, while the medium to long wavelength anomalies are possibly due to the combined effects of variations in the magnetic susceptibility and topography of the underlying basement and deeply seated intrusive bodies.

尼日利亚贝努埃海槽伪重力研究的初步结果
作为贝努埃海槽项目的一部分,正在对贝努埃海槽进行伪重力研究,这里介绍了这项研究的初步结果。利用等效层法对贝努埃海槽的若干航磁剖面进行了转换,得到了相应的伪重力剖面。对伪重力、航磁和重力剖面进行了定性解释和比较,以便找到在槽上观测到的短波长异常的可能来源。分析结果表明,短波长异常可能是由浅部较小的侵入体引起的,而中长波异常可能是下伏基底和深部侵入体磁化率和地形变化共同作用的结果。
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