Chemical Characteristics of Industrial Geological Parameters and Their Implications in Uranian Overview of Pa Lua - Pa Rong Area

Tran Le Chau, N. Phuong, N. T. Giang, Le Quyet Tam, Nguyen Tien Phu, Nguyen Dinh Than, Trinh Dinh Huan
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Abstract

This study investigated the geological properties of the uranium ore found in Pa Lua - Pa Rong area for potential industrial exploitation. A combination of field measurements, modeling and several mathematical approaches were employed to characterize the geological properties of the uranium ore. We found: i) The thickness of the ore bodies ranges from thin to medium, exhibiting varying degrees of instability (Vm = 83.8÷102.8%). The average U3O8 content indicates that the ore bodies belong to the poor ore type, with an unevenly distribution (Vc = 57.9÷100.9%); ii) The morphology and structure of the ore bodies are highly complex, exhibiting irregular variations. The thickness of the ore bodies shows a positive correlation with the uranium content in each body (R = 0.6-0.7); iii) The variograms of the U3O8 concentration and the thickness in various directions exhibit a spherical pattern, indicating an autogenous effect. The most significant variation in uranium content aligns with the dip direction (50°±12.5°), while the least variation aligns with the strike of the ore body (140°±12.5°). The variations in ore body thickness are more straightforward and consistent with those of the uranium content. In summary, these findings provide valuable insights into the characteristics of uranium ore in Pa Lua – Pa Rong area. The results contribute to a better understanding of the geological processes and can inform some effective exploration strategies for uranium resources in this region.  
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巴鲁—巴戎地区工业地质参数化学特征及其铀矿概况
研究了巴鲁—巴戎地区铀矿的地质性质,为工业开发提供了条件。结合现场测量、建模和几种数学方法来描述铀矿石的地质性质。我们发现:i)矿体的厚度范围从薄到中等,表现出不同程度的不稳定性(Vm = 83.8÷102.8%)。U3O8平均含量表明矿体属于贫矿型,且分布不均匀(Vc = 57.9÷100.9%);(2)矿体形态结构高度复杂,呈不规则变化。矿体厚度与各矿体铀含量呈正相关(R = 0.6 ~ 0.7);(3) U3O8浓度与厚度在不同方向上的变化曲线呈球形,表明存在自生效应。铀含量随矿体走向变化最显著(50°±12.5°),随矿体走向变化最小(140°±12.5°)。矿体厚度的变化更直接,与铀含量的变化一致。综上所述,这些发现对巴陆—巴戎地区铀矿体特征有重要的指导意义。研究结果有助于更好地认识该区的地质过程,为该区铀资源的有效勘探提供指导。
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