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Gamma-ray spectrometric investigation of north El-Tor area, southwestern Sinai, Egypt

机译:埃及西奈半岛西南部El-Tor地区的伽马射线光谱研究

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Interpretation was executed on the airborne and ground spectrometric data of Abu-Zeneima/Al-Tor area for verifying the significant anomalies as it contains important targets for prospective nuclear materials. Airborne spectrometric survey revealed that younger granites, are characterized by increase in the three main radioactive elements up to 5.4% K, 10?ppm eU and 33?ppm eTh. The western part of the study area includes sedimentary section which contains uranium-bearing phosphate beds. They are characterized by increase of airborne uranium concentration up to 14.2?ppm without potassium or thorium enrichment. The airborne image maps for eU/eTh and eU/K as well as ternary composite map revealed also that there is a promising U-anomaly, associated with the sedimentary section.Detailed ground spectrometric survey for the Cretaceous Nubian sandstone in Wadi Araba indicated that it is characterized by eU content reaches about 34?ppm, while eTh attains only about 9.8?ppm and potassium is 1.2%. Therefore, the eU/eTh ratio, reaches to a value of 3.4. The same sandstone bed in Abu - Durba Formation possesses eU values reach 67?ppm, whereas eTh values attain 38?ppm and average of potassium is 0.5%. The eU/eTh ratio is about 2, indicates also enrichment of uranium. The eU reaches a concentration of about 40?ppm in limestone of Matulla Formation whereas, the eTh values attains about 3?ppm and average K is 0.1%. Therefore, the eU/eTh ratio reached 13, due to the limestone is phosphatic. High eU value reaching to 80?ppm is recorded in the limestone facies of Sudr Formation, while the eTh values up to 11?ppm and potassium of about 0.9% are recorded. The eU/eTh ratio value reaching 7.3 indicates the high P2O5content. A high uranium content is recorded at the northeastern part of El-Qaa plain area in the Sudr Formation reaching 47?ppm, while low eTh values attaining 7.5?ppm and potassium of 0.1% are recorded.
机译:对Abu-Zeneima / Al-Tor地区的空中和地面光谱数据进行了解释,以验证重大异常,因为它包含潜在核材料的重要目标。机载光谱调查显示,年轻的花岗岩的特征在于三种主要放射性元素的增加,分别高达5.4%K,10?ppm eU和33?ppm eTh。研究区域的西部包括沉积部分,其中包含含铀的磷酸盐床。它们的特点是在不富集钾或th的情况下,空气中铀的浓度增加到14.2ppm。机载eU / eTh和eU / K的影像图以及三元复合图也显示出与沉积剖面有关的U异常现象。瓦迪阿拉巴白垩纪努比亚砂岩的详细地面光谱测量表明:其特征在于eU含量达到约34?ppm,而eTh仅达到约9.8?ppm,钾为1.2%。因此,eU / eTh比达到3.4的值。阿布-杜尔巴组的同一砂岩床的eU值达到67?ppm,而eTh值达到38?ppm,钾的平均值为0.5%。 eU / eTh比约为2,表明铀也富集。 Matulla组石灰岩中的eU达到约40?ppm的浓度,而eTh值达到约3?ppm,平均K为0.1%。因此,由于石灰石是磷酸盐,因此eU / eTh比达到13。 Sudr组的石灰岩相中记录到的高eU值达到80?ppm,而记录到的eTh值高达11?ppm,钾含量约为0.9%。 eU / eTh比值达到7.3表示P2O5含量高。 Sudr组El-Qaa平原区东北部的铀含量高,达到47?ppm,而eTh值低至7.5?ppm,钾含量为0.1%。

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