Asfahani J, Al-Hent R, Aissa M
Geology Department, Atomic Energy Commission, Damascus, Syria.
Appl Radiat Isot. 2008 Sep;66(9):1262-74. doi: 10.1016/j.apradiso.2008.01.018. Epub 2008 Feb 14.
The relationships between equivalent uranium (eU), eTh, K% and their ratios in the 11 lithological units determined by previous research in the Al-Awabed area, Northern Palmyrides, Syria have been analyzed in order to define their trend variations and evaluate the degree of uranium remobilization. Uranium favorability index U(I) and alteration-F indicators have been used in this research to characterize the different lithological units by following their radioactive element re-distribution and to determine their favorability as regards uranium potentiality. It was shown that uranium remobilization took place in all the lithological units, but to different degrees. This remobilization is qualified as weak, indicating that limited uranium redistribution is expected in the studied region. A plausible geological model is proposed for the uranium distribution, where the Abou Qila location is found to be favorable for uranium accumulation and merits further uranium exploration.
对叙利亚帕尔米拉北部地区Al-Awabed区域先前研究确定的11个岩性单元中的等效铀(eU)、钍等效物(eTh)、钾含量(K%)及其比率之间的关系进行了分析,以确定其趋势变化并评估铀的迁移程度。本研究中使用了铀有利指数U(I)和蚀变F指标,通过追踪放射性元素的重新分布来表征不同的岩性单元,并确定它们在铀潜力方面的有利程度。结果表明,所有岩性单元中均发生了铀迁移,但程度不同。这种迁移被认为是微弱的,这表明在研究区域内预计铀的再分布有限。针对铀的分布提出了一个合理的地质模型,其中发现Abou Qila地区有利于铀的富集,值得进一步进行铀勘探。