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首页> 外文期刊>Journal of African Earth Sciences >Basement configuration and lineaments mapping from aeromagnetic data of Gongola arm of Upper Benue Trough, northeastern Nigeria
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Basement configuration and lineaments mapping from aeromagnetic data of Gongola arm of Upper Benue Trough, northeastern Nigeria

机译:尼日利亚东北部上贝努槽的贡戈拉臂的航空磁数据绘成的地下室构造和构造

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摘要

The petroleum prospect evaluation of the Gongola arm of the Upper Benue Trough in the northeastern part of Nigeria has been undertaken through the analyses of High Resolution Aeromagnetic data (HRAM) acquired over the basin, with a view to determining sections of the basin having basement geometry, sedimentary thickness and structural framework among others that could support generation and preservation of the hydrocarbon resource. Processed, transformed and enhanced Total Magnetic Intensity (TMI) data were subjected to various analyses to define terrain geology, extract lineaments and delineate basement geometry, which were subsequently employed to generate basement model and structural framework of the basin. Most of the extracted lineaments trend ENE - WSW direction while Analytic Signal - Euler Deconvolution depth-weighting generate solutions which range in sediment thickness from 50 m above to over 5 km below the Minna reference datum, thus presenting undulating basement topography. Three sub-basins having depths in excess of 3 km, separated from each other by infra-basin subsurface basement highs, were delineated. The coexistence of considerably thick (3-5.7 km) sedimentary rock units and underlying structurally active basement rocks, assured geothermal gradient for organic matter maturation and guaranteed trapping of generated oil and gas within reservoirs' structural traps.
机译:通过分析在盆地上方采集的高分辨率航空电磁数据(HRAM),对尼日利亚东北部上贝努尔海槽的贡戈拉臂进行了石油前景评估,目的是确定盆地中具有地下室几何形状的部分,沉积厚度和结构框架等可以支持碳氢化合物资源的产生和保存。对经过处理,转换和增强的总磁强度(TMI)数据进行各种分析,以定义地形地质,提取线状体和描述地下室的几何形状,随后将其用于生成盆地的地下室模型和结构框架。大部分提取的地层趋向ENE-WSW方向,而解析信号-Euler反卷积深度加权生成的解决方案的沉积物厚度范围从Minna参考基准面以上50 m到低于Minna参考面5 km以上,因此呈现出起伏的地下室地形。划定了三个深度超过3 km的子盆地,这些子盆地之间由地下盆地地下地下室高点隔开。相当厚的(3-5.7 km)沉积岩单元与下伏的结构活跃基底岩并存,确保有机物质成熟的地热梯度,并确保将生成的油气捕获在储层的构造圈闭中。

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