尼日利亚Ilesha西南地区手数字化航磁数据的正反演建模

Robert Bassey, Peter O. Odong
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引用次数: 1

摘要

本文介绍了尼日利亚Ilesha SW的航磁资料解释结果。伊莱沙地质属于前寒武纪,位于尼日利亚基底杂岩之下。预计本区烃源岩深度较浅。结果表明,研究区内存在角闪岩、石英和片岩等常见岩石类型。对比例尺为1:5万的航磁图进行了手工数字化处理,并利用4.10.02版本的Potent软件进行了正演和反演建模。对野外资料进行定性和定量解释,结果显示研究区断裂带呈NE-SW向,异常体总磁强从负最小峰值-625.5 nT到正最大峰值179.43 nT,获得的磁源体最大至顶深度为34.2 m,最小深度为0.5 m。结果表明,在尼日利亚基底杂岩体的大部分地区,磁异常的深度较浅。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Forward and Inverse Modeling of Hand Digitized Aeromagnetic Data from Ilesha South West, Nigeria
Results of aeromagnetic data interpretation of Ilesha SW, Nigeria are presented here. The geology of Ilesha which is Precambrian falls under the basement complex of Nigeria. Depths to source rocks in this area are expected to be shallow. The results obtained revealed the presence of rocks such as amphibolites, quartz and schist which are the common rock types present in the study area. An aeromagnetic map of scale 1:50,000 was hand digitized, while forward and inverse modeling was achieved via the use of Potent, version 4.10.02. The field data were qualitatively and quantitatively interpreted and results showed NE-SW trending of the fault zone in the study area and anomalous bodies whose total magnetic intensity ranges from a minimum negative peak value of -625.5 nT to a maximum positive peak value of 179.43 nT. The maximum depth to top of the magnetic source body obtained is 34.2 m and minimum depth is 0.5 m. The results obtained indicate shallow depths to magnetic anomalies, as expected in most areas of the basement complex of Nigeria.
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