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首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Characterization of metal-bearing particles in groundwater from the Weilasituo Zn-Cu-Ag deposit, Inner Mongolia, China: Implications for mineral exploration
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Characterization of metal-bearing particles in groundwater from the Weilasituo Zn-Cu-Ag deposit, Inner Mongolia, China: Implications for mineral exploration

机译:中国内蒙古韦利亚托Zn-Cu-Ag矿床地下水中含金属颗粒的表征:矿产勘探的影响

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摘要

Nanoparticles in groundwater have important implications for facilitating the transportation of metals in groundwater and, to a certain extent, can reveal the geochemical conditions of the groundwater. Therefore, there is an increasing interest in analytical techniques that allow for in-depth characterization of nanoparticles in the groundwater and utilize these characteristics for geochemical prospecting. Metal-bearing particles in groundwater samples from deep-lying orebodies (referred to as "deep groundwater") of the Weilasituo Zn-Cu-Ag Deposit, Inner Mongolia, China and the groundwater from motor-pumped wells of a catchment basin around Weilasituo were chosen to study. Using high-angle annular dark-field scanning transmission electron microscopy (HAADF-STEM) and transmission electron microscopy (TEM) coupled with energy dispersive X-ray spectrometer (EDS), individual particles were characterized. Based on the TEM compositional and structural investigation, Ag-, Pb-, Cu-, Zn-, Sn-, As- and Mo-bearing particles were observed in the groundwater samples collected in the deep ore and the catchment basin. These metal-bearing particles are compositionally and structurally similar to the ore mineral/metal-bearing particles observed in the ore bodies and can directly reflect the ore-forming elemental characteristics, e.g., metallogenic element assemblage and mineralization type, of the Weilasituo deposit. The result indicates that the metal-bearing particles originating from the concealed ore bodies migrate via the groundwater flow and discharge to the catchment basin. This finding implies that the metal-bearing particle phases have great significances in facilitating the transportation of ore-related species and forming the geochemical anomalies in the groundwater. This field-scale study demonstrates that, by applying the analytical transmission electron microscopy, the nanocharacteristics of metal-particles can be utilized to improve the accuracy and sensitivity for geochemical mineral exploration.
机译:地下水中的纳米颗粒具有重要意义,以促进地下水中的金属运输,并且在一定程度上可以揭示地下水的地球化学条件。因此,对分析技术的兴趣越来越受到地下水中纳米颗粒的深入表征,并利用这些特征进行地球化学勘探。来自深层矿石的地下水样品中的金属含金颗粒(称为“深层地下水”)的Weilasituo Zn-Cu-Ag沉积物,中部蒙古,中国和地下水,来自Weilasituo的集水盆的热带泵井是选择学习。使用高角度环形暗场扫描透射电子显微镜(HAADF-STEM)和透射电子显微镜(TEM)与能量分散X射线光谱仪(EDS)相结合,表征各个颗粒。基于TEM组成和结构研究,在深矿石和集水区盆地收集的地下水样品中观察到Ag-,Pb,Cu-,Zn,Sn-,轴承颗粒。这些金属含金颗粒在矿体中观察到的矿石/金属/金属/金属含颗粒的构成和结构类似,并且可以直接反映Weilasituo沉​​积物的形成元素特征,例如成矿元素组合和矿化型。结果表明,源自隐藏矿体的金属承载颗粒通过地下水流动迁移到集水盆地。该发现意味着金属含颗粒相对于促进与矿石相关物种的运输具有重要意义,并在地下水中形成地球化学异常具有重要意义的重要意义。该场比例研究表明,通过施加分析透射电子显微镜,可以利用金属颗粒的纳米特征来提高地球化学矿物勘探的准确性和灵敏度。

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