Keffi Sheet 208N Angwan Zakara地质和水文地球物理调查。尼日利亚中北部东部

C. Okeke, B. Jatau, A. Kana
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引用次数: 1

摘要

本研究对尼日利亚中北部纳萨拉瓦州卡鲁地方政府Angwan Zakara及其周边地区的地下水前景/潜力进行了地质和水文地球物理评价。研究区面积25平方公里。该地区位于尼日利亚中北部基底杂岩之下,由中粒黑云母花岗岩、黑云母片麻岩、千层岩和不可测白云母片岩组成,构造特征为节理、脉、片理、断裂和北西-东向捕虏体。在研究区使用Omega电阻率测深仪、GPS12 Garmix进行了49次垂直电测深,最大电缆展布AB/2=100m, MN/2=5m。使用IXID软件对现场数据进行解释,进行定量分析。利用SURFER 8软件制作了真电阻率图、压测图、基底电阻率图和深至基底图,并进行了定性解译。IXID解译结果显示,从获取的数据中得到了5种曲线类型,A、H、KH、AH和HK曲线类型占主导地位。研究区至基底深度为20 ~ 90m。这显示了良好的地下水潜力。研究区发育表层土、红土、粘土、风化/断裂基底等4-7个岩性序列,寄主岩为黑云母花岗岩、石英岩和片麻岩。结果表明:水的流动方向为5个脊R1 ~ r5和4个凹陷d1 ~ d4,脊的容水方向为R1和R2:NW-SE;R3 N-S、R4、NE-SW、R5;南临。制作地电剖面,并与研究区地质进行对比,发现两者吻合较好。在此基础上,将研究区划分为地下水潜力好、中、差3个区。
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Geological and Hydrogeophysical Investigation of Angwan Zakara, Keffi Sheet 208N.E of North Central Nigeria
The geological and hydrogeophysical assessment of the groundwater prospect/potential in Angwan Zakara and its environs, Karu Local Government, Nasarawa State, North-Central, Nigeria has been carried out in this study. The study area covers 25km2.The area is underlain by the Basement Complex of the North-Central Nigeria consisting of Medium grained biotite granite, biotite gneiss, phyllite and un-mappable muscovite schist with structural features such as joints, veins, foliation, faults, and xenoliths trending NW-SE direction. Forty Nine (49) Vertical Electrical Sounding were carried out in the study area using Omega Resistivity Terrameter, GPS12 Garmix with a maximum cable spread of AB/2=100m and MN/2=5m. The results obtained from the field data were interpreted using IXID Software for quantitative analysis. True resistivity map, piezometric map, basement resistivity map and depth to basement map were prepared and interpreted using computer software for qualitative analysis (SURFER 8). From the IXID interpreted results, five (5) curve types were obtained from the acquired data namely A, H, KH, AH, and HK curve types are the dominant. The study area showed depth to basement ranges from 20-90m. That revealed good groundwater potential. The study area revealed 4-7 lithologic sequences consisting of top soil, laterite, clay, weathered/ fractured basement however the host rocks in the study area are biotite granite, quartzite and schistose-gneiss. The results obtained shows that the direction of water flows revealed five ridges R1-R5 and four depressions D1-D4 with receptacles trends of the ridges are R1 and R2:NW-SE; R3 N-S, R4 : NE-SW and R5; E-W. The geoelectric sections were produced and correlated with the geology of the study area and it was found to be in conformity with the each other. Based on this, the study area is zoned into three namely good, moderate and poor groundwater potential zones.
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