首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >Stream sediment geochemical patterns around an ancient gold mine in the Wadi El Quleib area of the Allaqi region, south Eastern Desert of Egypt: Implications for mineral exploration and environmental studies
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Stream sediment geochemical patterns around an ancient gold mine in the Wadi El Quleib area of the Allaqi region, south Eastern Desert of Egypt: Implications for mineral exploration and environmental studies

机译:在埃及南沙漠东南沙漠瓦地区瓦迪·卢比德地区围绕古金矿周围的泥沙地球化学模式:对矿物勘探和环境研究的影响

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摘要

The investigation of geochemical patterns in stream sediments around the newly discovered ancient gold mine in the Wadi El Quleib area is aimed at economic evaluation and environmental assessment of catchment sediments. For these reasons, forty stream sediment's composite samples were collected from the area covered by the metamorphosed ultramafic and their derivatives, volcanogenic metasediments, granitoid plutons, sand stones, and unconsolidated sediments. Fifty three chemical elements were analyzed using inductively coupled plasma mass spectrometry. They were processed using various mathematical computations, graphical plots, and mapping techniques. The results revealed that the multiple populations within data set were caused by natural and ancient mining activities. Both geogenic and anthropogenic sources could influence On the dispersion of the elements of interest in the stream sediments. Despite sediments' materials were predominantly generated from metabasic and ultramafic provenance rather than mixed and fiesic sources, and the area may have been subjected to more than one weathering cycle, they did not follow the sedimentary sorting and recycling trend. The lack of Au content and the negative correlation of Au with other elements are due to ancient human works and thus, the combined elements Ag + As, Ag + Hg, and Ag + Hg + As are considered the pathfinder for Au mineralization. The metamorphosed ultramafic and their derivatives, volcanogenic metasediments and their thrust contact host Au-mineralization, Cr-mineralization, and Ni-bearing minerals. Environmentally, the low values of contamination degrees and potential ecological risk indices of heavy metal(loid)s indicated that the sediment materials are good in quality and possess no actual hazard to human health. In general, the study area is more promising for Au mineralization and accepted as safe environment for the urban renewal purposes and land-use management in the future. (C) 2016 Published by Elsevier B.V.
机译:在Wadi El-Quleib地区新发现的古金矿周围河流沉积物的地球化学模式调查旨在对集水区沉积物进行经济评估和环境评估。由于这些原因,从变质超镁铁质及其衍生物、火山成因变质沉积物、花岗质深成岩体、砂岩和松散沉积物覆盖的区域收集了40个河流沉积物的复合样品。用电感耦合等离子体质谱法分析了53种化学元素。他们使用各种数学计算、图形绘制和绘图技术进行处理。结果表明,数据集中的多个种群是由自然和古代采矿活动造成的。地质和人为来源都可能影响河流沉积物中感兴趣元素的分散。尽管沉积物的物质主要来源于变质基性和超镁铁质物源,而不是混合源和火山源,而且该地区可能经历了一个以上的风化循环,但它们没有遵循沉积分选和再循环趋势。金含量的缺乏以及金与其他元素的负相关性是由于古代人类的工作,因此,组合元素Ag+As、Ag+Hg和Ag+Hg+As被认为是金矿化的探索者。变质超镁铁质及其衍生物、火山成因变质沉积物及其逆冲接触带承载着金矿化、铬矿化和含镍矿物。环境方面,重金属污染程度和潜在生态风险指数(loid)值较低,表明沉积物材料质量良好,对人类健康没有实际危害。总的来说,研究区域更有可能进行金矿化,并被认为是未来城市更新和土地使用管理的安全环境。(C) 2016年由爱思唯尔B.V.出版。

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