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2.5D Modelling of Aeromagnetic Data and their Mining Implications over the Ngaoundere Area (Adamawa Province, Cameroon)

机译:Ngaoundere地区(喀麦隆阿达玛瓦省)的航空磁数据的2.5D建模及其采矿意义

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This study is based on the analysis and interpretation of aeromagnetic data using version 8.4 of the Geosoft Oasis Montaj Software, to map the subsurface or deep geological structures that affected the geological formations of the Ngaoundere area. The use of the standard aeromagnetic methods made it possible to draw up the maps of the residual magnetic field reduced to the equator (RTE), the horizontal gradient (HG), the analytical signal (AS) and that of the Euler solutions (ED) to find the main magnetic facies corresponding to these structures. The geological formations of the studied area thus appear to be intensely fractured by a NE-SW (N45°E) and ENE-WSW (N70°E) main orientation fault system, the depth of which has been estimated by combining the three-analytical methods HG, AS and ED. Advanced magmatic map analysis revealed dikes associated with vertical faults in the studied area. The development of an interpretative geological map taking into account the basic geology, the deep faults, the identified dikes and the mineralization index made it possible to extract a correlation between geological structures and mineralization of the studied area. The 2.5D modelling of two magnetic profiles plotted on the reduced residual map at the equator was performed to approximate the geometry and depth of the dikes sector, which are potential sources of mineralization here.
机译:这项研究基于使用Geosoft Oasis Montaj软件8.4版对航空磁数据进行的分析和解释,以绘制出影响Ngaoundere地区地质构造的地下或深部地质结构。使用标准的航空磁方法,可以绘制减少到赤道(RTE),水平梯度(HG),分析信号(AS)和欧拉解(ED)的剩余磁场的图。寻找与这些结构相对应的主要磁性相。因此,研究区的地质构造似乎被NE-SW(N45°E)和ENE-WSW(N70°E)主方向断层系统强烈断裂,其深度已通过结合三分析法进行了估算。方法HG,AS和ED。先进的岩浆图分析揭示了与研究区域内垂直断层有关的堤防。考虑到基本地质,深层断层,确定的堤防和矿化指数的解释性地质图的开发,使得可以提取研究区域的地质结构与矿化之间的相关性。对在赤道处的缩小残留图上绘制的两个磁剖面进行2.5D建模,以近似堤防区段的几何形状和深度,这是这里潜在的矿化来源。

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