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首页> 外文期刊>Applied radiation and isotopes: including data, instrumentation and methods for use in agriculture, industry and medicine >Aerial spectrometric survey for localization of favorable structures for uranium occurrences in Al-Awabed area and its surrounding (Area-3), Northern Palmyrides -Syria.
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Aerial spectrometric survey for localization of favorable structures for uranium occurrences in Al-Awabed area and its surrounding (Area-3), Northern Palmyrides -Syria.

机译：空中光谱测量法，用于在北棕榈yr-叙利亚的Al-Awabed地区及其周边地区（Area-3）中形成铀有利构造。

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摘要

A scored lithological map including 11 radiometric units is established through applying a factor analysis approach to aerial spectrometric data of Area-3, Northern Palmyrides, Syria. Regional uranium migration trends have also been estimated by using the airborne spectrometric data of Area-3, where different regional maps explaining the migration trends have been established. It was found that the four lithological phosphatic units P1, P2, P3 and P4 are the main uranium sources in the study region, where the uranium migration is in an outward direction. The other seven lithological units C1, C2, C3, M1, M2, M3 and M4 are successively and differentially enriched by uranium during the geological evolution of the crust, where uranium migration is generaly in an inward direction. The combination of the obtained uranium migration results with the dominant geological and tectonic conditions allows the proposition of a plausible scenario of six steps, which explain the different geological processes taking place in the study area. Favorable transverse structures for uranium occurences have been localized and qualified as being the most important for prospecting. More detailed exploration activities are needed in the study area to evaluate the potential of such structures as a function of depth. The proposed model could be applicable to similar phosphatic environments.
机译：通过将因子分析方法应用于叙利亚北部Palmyrides的Area-3的航空光谱数据，建立了包括11个辐射计量单位的刻蚀岩性图。还通过使用Area-3的航空光谱数据估算了区域铀迁移趋势，并在其中建立了解释迁移趋势的不同区域图。结果发现，四个岩性磷化单元P1，P2，P3和P4是研究区域中铀的主要来源，铀的迁移是向外的。在地壳的地质演化过程中，其他七个岩性单元C1，C2，C3，M1，M2，M3和M4依次并不同程度地被铀富集，其中铀的迁移通常向内。将获得的铀迁移结果与主要的地质和构造条件相结合，可以提出一个合理的方案，该方案可分为六个步骤，这可以解释研究区域内发生的不同地质过程。有利于铀发生的横向结构已被本地化，并被认为是最重要的勘探手段。研究区域需要进行更详细的勘探活动，以评估这种结构作为深度函数的潜力。所提出的模型可以适用于类似的磷酸环境。

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