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首页> 外文期刊>Journal of South American earth sciences >Quartz resources in the Serra de Santa Helena formation, Brazil: A geochemical and technological study
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Quartz resources in the Serra de Santa Helena formation, Brazil: A geochemical and technological study

机译:巴西Serra de Santa Helena地层中的石英资源:地球化学和技术研究

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摘要

This study presents an evaluation of Brazilian quartz deposits of Corinto and Olhos D'agua, in Minas Gerais State, as potential high purity raw material for the production of silica glass. Both deposits are part of the Serra de Santa Helena formation, which holds other quartz deposits. Several quartz samples from these mines were analyzed to evaluate their chemical purity, by determination of the content of trace elements by ICP-MS after acid digestion. The technological characteristics of the ores after flame-fusion into silica glass were evaluated according to their bubble generation and UV transparency. The results indicate that silica glass with chemistry suitable for crucible applications can be obtained from materials of both mines, and even optical grade silica glass can be manufactured using transparent ore from one of the mines. In addition, this work explores the trace elements composition of each mine, as well as their fluid inclusions, and characterizes the mines as being of hydrothermal origin. Small differences in the physical and chemical characteristics of quartz that could affect the technological behavior of the ores are related to the geological history of the mines and provide interesting insights regarding the exploration of other quartz resources within the same geological formation.
机译:这项研究提出了对米纳斯吉拉斯州Corinto和Olhos D'agua的巴西石英矿床的评估,这些矿床是生产石英玻璃的潜在高纯度原材料。这两个矿床都是Serra de Santa Helena地层的一部分,该地层还有其他石英矿床。酸消解后,通过ICP-MS测定痕量元素的含量,对这些矿山的几个石英样品进行了分析,以评估其化学纯度。根据矿石的气泡生成和紫外线透明性,对矿石进行火焰融合后的技术特性进行了评估。结果表明,可以从两个矿山的材料中获得具有适用于坩埚应用的化学性质的石英玻璃,甚至可以使用其中一个矿山的透明矿石来制造光学级石英玻璃。此外,这项工作探索了每个矿山的痕量元素组成及其流体包裹体,并将这些矿山归类为热液来源。石英的物理和化学特征上的细微差异可能会影响矿石的技术行为,这与矿山的地质历史有关,并为探索同一地质构造内的其他石英资源提供了有趣的见解。

著录项

  • 来源
    《Journal of South American earth sciences》 |2014年第12期|328-338|共11页
  • 作者单位

    Department of Materials Engineering, Faculty of Mechanical Engineering, Campinas State University (UNICAMP), Rua Mendeleiv, 200, Cidade Universitaria Zeferino Vaz, Campinas, Brazil,Rua 3, n°2131, Rio Claro, Sao Paulo 13500-163, Brazil;

    Department of Integrated Systems, Faculty of Mechanical Engineering, Campinas State University (UNICAMP), Rua Mendeleiv, 200, Cidade Universitaria Zeferino Vaz, Campinas, Brazil;

    Department of Materials Engineering, Faculty of Mechanical Engineering, Campinas State University (UNICAMP), Rua Mendeleiv, 200, Cidade Universitaria Zeferino Vaz, Campinas, Brazil;

    Institute of Geosciences, State University of Campinas (UNICAMP), Rua Joao Pandia Calogeras, 51, Cidade Universitaria Zeferino Vaz, Campinas, Brazil;

    Department of Materials Engineering, Faculty of Mechanical Engineering, Campinas State University (UNICAMP), Rua Mendeleiv, 200, Cidade Universitaria Zeferino Vaz, Campinas, Brazil;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Quartz; Trace elements in quartz; Resources for silica glass; High purity quartz;

    机译:石英;石英中的微量元素;石英玻璃资源;高纯石英;

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