绘制第三大陆末端(ct3)地层的放射性地图:尼亚美地区三姊妹地层(非洲西部克拉通东缘,伊利姆梅登盆地)的情况

Sofiyane Abdourahamane Attourabi, Mallam Mamane Hallarou, Assagaye Agaissa, Mahamane Moustapha Sanda Chekaraou, Gambo Ranaou Noura, Lawali Idi Chamsi
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摘要

大陆末期 3(Ct3)地层主要位于西非克拉通的比里米亚基底上,与尼亚美地区(尼日尔西部)Iullemmeden 盆地最后的充填沉积相吻合。这项研究的总体目标是绘制尼亚美三姊妹山地区地表辐射测量图。采用的方法包括实地考察和实验室工作,并使用 Surfer 软件对辐射测量数据进行处理。三姊妹山地区的放射性值介于 5 至 25 震荡/秒(C/s)之间。高放射性值(15 至 25 c/s)记录在上部,与胸板相对应。低放射性值(5 至 15 c/s)在基底层测得,与粘土和冲积层相对应。这种放射性被认为是由于这些露头中的痕量铀造成的。
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MAPPING RADIOACTIVITY IN CONTINENTAL TERMINAL 3 (CT3) FORMATIONS: THE CASE OF THE THREE SISTERS, NIAMEY REGION (EASTERN EDGE OF THE WEST AFRICAN CRATON, ILLUMMEDEN BASIN)
The Continental Terminal 3 (Ct3) formations, which rest in major unconformity on the Birimian basement of the West African Craton, correspond to the last filling deposits of the Iullemmeden basin in the Niamey region (West, Niger). The general objective of this study is to produce a surface radiometric map of the Niamey Three Sisters Hills area. The methodology used included field and laboratory work, with radiometric data processed using Surfer software. Radioactivity values in the Three Sisters area ranged from 5 to 25 shocks per second (C/s). High radioactivity values (15 to 25 c/s) are recorded in the upper terms, corresponding to the breastplates. Low values of radioactivity (5 to 15 c/s) are measured in the basal layers, corresponding to clays and alluvium. This radioactivity is thought to be due to trace amounts of uranium in these outcrops.
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