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Gamma-Ray Spectrometry and Induced Polarization Studies for El Atshan-II Uranium Prospect Area, Central Eastern Desert, Egypt

机译:埃及中部东部沙漠El Atshan-II铀矿勘探区的伽马射线能谱和诱导极化研究

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Gamma-ray spectrometry and induced polarization (IP) studies were carried out to determine the radioactive anomalous zones and to follow their lateral and vertical extensions in El Atshan-II uranium prospect area, central Eastern Desert, Egypt. This area and its surroundings are covered by different Precambrian basement rocks, which intruded by younger bostonite rock, andesite dykes and carbonate veins. Data of the gamma-ray spectrometry have been analyzed qualitatively and quantitatively by applying specific interpretation techniques. These data revealed a wide radioactivity range oscillating from 15.0 to 2362.0 Ur, 0.5 to 307.2 ppm, 0.1 to 55.1 ppm and 0.3 to 22.0% for the total count (Tc), equivalent uranium (eU), equivalent thorium (eTh) and potassium (K), respectively. The constructed radioelement concentration maps and eU-composite image of the study area showed that the anomalously high radioactivity levels are mainly associated with outcrops of the bostonite rock. The induced polarization data were mathematically inverted to produce the true resistivity and chargeability values of cross-sections below the surveyed lines traverse in the area. The resistivity values are varied both vertically and horizontally from 7.83 to more than 1042.0 ohm·m, while the chargeability values are ranged from 0.195 to more than 204.0 mV/V, suggesting variation of the rocks facies and mineralizations. Integration of the resistivity and chargeability data indicates the presence of some mineralized zones, mainly associated with the bostonite rock, with depths varied from the near-surface to more than 70 m. Therefore, a core drilling is recommended at some stations along three selected profiles to a depth of 70 - 100 m to test the depth, structural model and grade of mineralization in the area.
机译:在埃及东部沙漠中部的El Atshan-II铀矿勘探区,进行了伽马射线能谱和诱导极化(IP)研究,以确定放射性异常区并跟踪其横向和垂直方向的扩展。该地区及其周围地区被不同的前寒武纪基底岩所覆盖,这些基底岩被较年轻的波士顿岩,安山岩堤和碳酸盐岩脉侵入。通过应用特定的解释技术,已对定性和定量分析了伽马射线光谱数据。这些数据显示总放射性(Tc),当量铀(eU),当量th(eTh)和钾的放射性范围宽广,从15.0至2362.0 Ur,0.5至307.2 ppm,0.1至55.1 ppm和0.3至22.0% (K)。构造的放射性元素浓度图和研究区的eU复合图像表明,异常高的放射性水平主要与辉石岩的露头有关。将感应的极化数据数学上反转,以产生该区域中遍历的测量线以下的横截面的真实电阻率和荷电率值。电阻率值在垂直和水平方向上都从7.83到1042.0 ohm·m以上变化,而带电率值在0.195到204.0 mV / V以上的范围内变化,表明岩石相和成矿作用有所变化。电阻率和带电性数据的综合表明,存在一些矿化带,主要与硼铁矿岩石有关,其深度从近地表到70 m以上不等。因此,建议在某些站点沿三个选定的剖面进行岩心钻探,深度为70-100 m,以测试该区域的深度,构造模型和成矿等级。

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