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A review of stratigraphic surfaces generated from multiple electrical sounding and profiling

机译:多次电测深和剖面生成的地层表面综述

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摘要

In this work, we investigate the accuracy of stratigraphic surfaces derived from multiple electrical sounding and traversing. Eight (8) VES stations with AB/2 of > 80 m each and three (3) Wenner profiling of > 120 m each were used for this investigation. The three principal surfaces interpreted include conglomeratic sand (top layer}, sandstone (presumably compacted) and clayey sandstone. These rocks are correlated to the Ise Formation of eastern Dahomey Basin. Our result shows that widely-spaced VES are error-prone and may result in misinterpretation of subsurface resistivity and rock boundaries. Smaller spacing between VES stations can effectively detect minute resistivity anomalies. On the other hand, the inversion method used for interpretation of profiling data can influence the final resistivity values. We propose the criteria for generating strati-graphic surfaces to include (a) adequate geological mapping (b) small electrode spacing for profiling (c) closely-spaced VES stations and profiling lines (d) interpolation of thickness and resistivity in multiple direction and (e) the use of drill hole logs to tie VES models.
机译:在这项工作中,我们研究了由多次电测深和穿越得到的地层表面的准确性。八(8)个VES站,AB / 2每个> 80 m,三(3)个Wenner曲线,每个> 120 m,用于本研究。解释的三个主要表面是砾岩(顶层),砂岩(可能是压实的)和黏土砂岩,这些岩石与达荷美盆地东部的伊势组有关,我们的结果表明,大范围的VES容易出错,可能导致在错误解释地下电阻率和岩石边界时,较小的VES站间距可以有效地检测微小的电阻率异常;另一方面,用于解释剖面数据的反演方法会影响最终的电阻率值。图形表面包括(a)足够的地质图(b)较小的电极间距以进行仿形(c)间距较近的VES测站和仿形线(d)沿多个方向插入厚度和电阻率,以及(e)使用钻孔测井绑定VES模型。

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