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Vertical Electrical Sounding Investigation in East River Nile Area (Khartoum State), Sudan
作者姓名:EldawiMG  FarwaAG  LiuTianyou
作者单位:[1]FacultyofGeophysicsandSpaceInformation,ChinaUniversityofGeosciences,Wuhan430074 [2]DepartmentofGeology,FacultyofScience,UniversityofKhartoum,Sudan
摘    要:Vertical electrical sounding (VES) was carried out in the east of the River Nile. The main objectives of the resistivity survey are to determine the types and thicknesses of sedimentary units in the area, to define the contact separating the sediments from the crystalline basement complex, and to determine the structural features of the subsurface formations. Several local depressions, whose maximum depth to the Imsement surface is about 160 m, are revealed as an outcome of the VES method, and suggested to have been infilled with undifferentiated units of the Nubian Group in particular Omdurman Formation. Thus, a depth to the basement complex is calculated and the associated structural map of the east of the River Nile is drawn. The map is useful for the groundwater drilling, as far as the presence or absence of the aquifer is concerned.

关 键 词:探通术  东尼罗河  苏丹  研究  区域地质学  蓄水层

Vertical Electrical Sounding Investigation in East River Nile Area (Khartoum State),Sudan
EldawiMG FarwaAG LiuTianyou.Vertical Electrical Sounding Investigation in East River Nile Area (Khartoum State),Sudan[J].Journal of China University of Geosciences,2003,14(4):368-373.
Authors:Eldawi M G  Farwa A G  Liu Tianyou
Abstract:Vertical electrical sounding (VES) was carried out in the east of the River Nile. The main objectives of the resistivity survey are to determine the types and thicknesses of sedimentary units in the area, to define the contact separating the sediments from the crystalline basement complex, and to determine the structural features of the subsurface formations. Several local depressions, whose maximum depth to the basement surface is about 160 m, are revealed as an outcome of the VES method, and suggested to have been infilled with undifferentiated units of the Nubian Group in particular Omdurman Formation. Thus, a depth to the basement complex is calculated and the associated structural map of the east of the River Nile is drawn. The map is useful for the groundwater drilling, as far as the presence or absence of the aquifer is concerned.
Keywords:VES method  basement complex  structural features  
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