Investigation of Geology and Hydro-geophysical Features Using Electromagnetic and Vertical Sounding Methods for Abu Zabad Area, Western Kordofan State, Sudan

E. A.B, M. M.A
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Abstract

The geology and hydro-geophysical features can aid in identifying borehole location. The study aims to investigate groundwater aquifers and best location of boreholes in the crystalline basement area of Abu Zabad near El Obeid Southwest, Sudan. The study area is underlain by two aquifers formations from Precambrian age. The oldest units of basement complex of area under investigation consist of metamorphic rocks including gneiss, schist, and quartzite. The geophysical methods electromagnetic (EM) and vertical electrical sounding (VES) surveys showed that best aquifers yield for construction of boreholes are in weathering and fractures formation. The EM results revealed that structural features are significant for groundwater potential and interpretation of the VES data also revealed four geo-electric layers, but generally two distinct lithologic layers, which include Superficial deposit and bedrock-basement respectively. The curves generated from the data revealed H curve and HK curve, and thickness of these layers varies from 15 m to 50 m in the area. The aquifer thickness range from 20 m to 30 m. The study concludes that these techniques are suitable for identifying borehole location in the basement rock in Abu Zabad Area Sudan.
苏丹西科尔多凡州Abu Zabad地区电磁与垂直测深地质与水文地球物理特征研究
地质和水文地球物理特征有助于确定井眼位置。该研究旨在调查苏丹El Obeid西南附近Abu Zabad结晶基底区的地下水含水层和钻孔的最佳位置。研究区下有两个前寒武纪的含水层。研究区最古老的基底杂岩单元由片麻岩、片岩和石英岩等变质岩组成。地球物理方法、电磁(EM)和垂直电测深(VES)调查表明,在风化和裂缝地层中,最适合钻孔施工的含水层产量。EM结果显示,构造特征对地下水潜力具有重要意义,而VES数据的解释也揭示了四个地电层,但总体上分为两个不同的岩性层,分别为浅层沉积层和基岩-基底层。数据生成的曲线为H曲线和HK曲线,厚度在15 ~ 50 m之间。含水层厚度在20 ~ 30 m之间。研究表明,这些技术适用于苏丹阿布扎巴德地区基底岩的井眼定位。
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