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High resolution airborne radiometric and magnetic studies of ilesha and its environs, southwestern Nigeria

机译:尼日利亚西南部伊莱沙及其周边地区的高分辨率机载辐射和磁学研究

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The study of the nature of distribution of natural radioelements in Ilesha and its environs with its geological structure has been studied using aeroradiometric data. Aeromagnetic data have also been subjected to three automated gradient techniques to delineate the sub-surface structure of the study area. From the study, it can be found that maximum values of “eU” (ppm) and “eTh” (ppm) fall within the branded gneiss, whereas the maximum value of K (%) falls within porphyritic granite regions. eTh had the highest radioactive content. The environmental dose rate of Ilesha was between 0.1817 and 3.9296 msv/yr. Although there were extreme values, but the mean dose rate was 0.522 ± 0.310 msv/yr (within acceptable safe limit of 1.0 msv/yr). eU/K, eU/eTh and eTh/K ratios were analysed for enrichment or depletion of radioisotopes. eU/eTh >1 showed uranium depletion, while eTh >2 showed eTh enrichment. The magnetic intensity values ranged from -79.41 to 140.93 nT. The horizontal gradient method (HGM) and analytic signal amplitude (ASA) revealed that depth to magnetic sources ranged from 0.478 to 4.112 km and 0.348 to 2.551 km, respectively, whereas local wavenumber (LWN) depth ranged from 0.478 to 5.48 km, which overestimated those compared using HGM and ASA functions. The apparent susceptibility ranged from -0.00325 to 0.00323 SI, showing that ferromagnetic and diamagnetic mineral ranges control apparent susceptibility in Ilesha.
机译:利用航空辐射数据研究了伊莱沙及其周围地区自然放射性元素分布的性质及其地质结构。航磁数据还经过了三种自动梯度技术来描绘研究区域的地下结构。从研究中可以发现,“ eU”(ppm)和“ eTh”(ppm)的最大值落在品牌片麻岩内,而K(%)的最大值落在斑岩质花岗岩区域内。 eTh的放射性含量最高。 Ilesha的环境剂量率在0.1817和3.9296 msv / yr之间。尽管存在极限值,但平均剂量率为0.522±0.310 msv / yr(在1.0 msv / yr的可接受安全限值内)。分析了eU / K,eU / eTh和eTh / K的比率,以确定放射性同位素的富集或耗尽。 eU / eTh> 1显示铀贫化,而eTh> 2显示eTh富集。磁强度值介于-79.41至140.93 nT之间。水平梯度法(HGM)和分析信号幅度(ASA)表明,磁源深度分别为0.478至4.112 km和0.348至2.551 km,而局部波数(LWN)深度为0.478至5.48 km,这被高估了那些使用HGM和ASA功能进行了比较。表观磁化率在-0.00325至0.00323 SI之间,表明铁磁性和反磁性矿物范围控制了伊莱沙岛的表观磁化率。

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