利用航磁资料估算尼日利亚阿南布拉盆地部分地区的构造模式和沉积厚度

Priscilla E. Ikioda, C. O. Ofoegbu, E. Uko, O. S. Ayanninuola
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摘要

摘要分析了阿南布拉盆地部分地区的航磁资料,以确定该盆地的结构模式和沉积厚度。研究区域由301(Udi)、302(Nkalagu)、312(Okigwe)和313(Afikpo)表上的高分辨率航磁数据覆盖,位于纬度5o30'0''-6o30''和经度7o0''-8o0''之间。将整个区域划分为25个重叠块,每个块37.2km2,并进行2D能谱分析。对总磁场强度数据进行过滤和分析技术,以确定结构模式、矿化潜力、基底深度和沉积厚度的变化。使用垂直导数生成的结构图显示,该地区的主要结构方向为ENE-WSW走向,次要走向为NW至SE方向,分布在整个地区。这些结构是研究区域内各种近表面磁侵入的结果。光谱分析结果显示,该区有深部和浅部两个深度层,深部异常源到磁基底的深度在3.3km到4.84km之间,平均深度为3.99km,而浅部磁源的深度在0.46km到0.67km之间,均值为0.56km。该区域的矿化模式遵循ENE-WSW方向。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of The Structural Pattern and Sedimentary Thickness Over Part Of Anambra Basin, Nigeria Using Aeromagnetic Data
Abstract Aeromagnetic data acquired over part of the Anambra Basin is analyzed to determine the structural pattern and sedimentary thickness of the basin. The study area is covered by high resolution aeromagnetic data on sheets 301 (Udi), 302 (Nkalagu), 312 (Okigwe) and 313 (Afikpo), and lies between latitudes 5o30’0’‘-6o30’0’‘ and longitudes 7o0’0”-8o0’0”. The whole area was divided into 25 overlapping blocks of 37.2km2 each and a 2D energy spectral analysis was carried out. Total magnetic intensity data was subjected to filtering and analytical techniques to determine the structural pattern, mineralization potential, depth to the basement, variation in the sedimentary thickness. The structural map generated using the vertical derivatives shows that the major structural orientation of the area is in the ENE-WSW trend and the minor trend is the NW to SE direction widespread all over the area. These structures are as a result of the various near-surface magnetic intrusion within the study area. The spectral analysis result shows two depth layers, the deep and the shallow depth, the depth to magnetic basement for the deep anomalous source ranges from 3.3km to 4.8 4km with an average depth of 3.99km, while the depth to shallow magnetic sources ranges between 0.46km to 0.67km and an average of 0.56km within the area. The mineralization pattern in this area follows the ENE-WSW direction.
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