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Raman I Do – Raman Spectroscopy for the Mineralogical Characterisation of Banded Iron Formation and Iron Ore

机译:拉曼一世–拉曼光谱学用于带状铁矿和铁矿石的矿物学表征

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摘要

The value of Raman spectroscopy to undertake mineral and chemical characterisation of ironrnores was assessed by applying the technique to representative samples of banded iron-formationsrn(BIF) and a BIF-derived, martite-goethite ore. The common iron oxides haematite, magnetite andrngoethite as well as gangue minerals such as quartz and carbonates all show distinct Raman spectrarnthat enables these phases to be easily detected and mapped in situ for either samples preparedrnas polished blocks or unprepared material. Raman spectroscopy also offers the potential of inrnsitu chemical characterisation. Shifts in the excitation bands of carbonate detected in BIF werernrelated to the Mg content of Fe-carbonate and confi rmed the fi rst world-wide occurrence of a highrnMg-bearing siderite (pistomesite) in BIF.rnThe discriminatory power of Raman spectroscopy coupled with the potential of the techniquernto offer large-scale (volumetric) characterisation of iron ore will be of great value not only to thernexisting BID and CID ore types, but also to the newly emerging magnetite iron deposits (MID).
机译:拉曼光谱法对铁矿的矿物和化学特征进行了评估,方法是将该技术应用于带状铁矿(BIF)和BIF衍生的马氏体-针铁矿矿石的代表性样品中。常见的氧化铁赤铁矿,磁铁矿和菱铁矿以及脉石矿物(例如石英和碳酸盐)都显示出独特的拉曼光谱,使这些相可以很容易地被检测到并在原位绘制,用于样品制备的抛光块或未制备的材料。拉曼光谱法还提供了原位化学表征的潜力。在BIF中检测到的碳酸盐激发带的变化与碳酸Fe中的Mg含量有关,并确认了BIF中首次出现高含Mg菱铁矿(Pistomesite)的拉曼光谱。提供铁矿石大规模(体积)表征技术的潜力,不仅对现有的BID和CID矿石类型,而且对新兴的磁铁矿(MID)都具有巨大的价值。

著录项

  • 来源
    《Iron ore 2011》|2011年|p.345-349|共5页
  • 会议地点 Perth(AU)
  • 作者

    E R Ramanaidou; M A Wells;

  • 作者单位

    Research Stream Leader Carbon Steel Materials – CSIRO Minerals Down Under Flagship, CSIRO ARRC, PO Box 1130, Bentley WA 6102. Email: Erick.Ramanaidou@csiro.au;

    CSIRO Minerals Down Under Flagship, CSIRO ARRC, PO Box 1130, Bentley WA 6102. Email: Martin.Wells@csiro.au;

  • 会议组织
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 铁矿石;
  • 关键词

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