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The ironsands studied in this work primarily consist of titanomagnetite (TTM, Fe3−xTixO4) and titanomagnetite-hematite (TTH, Fe2−yTiyO3) as the dominant mineral phases. The ironsands are largely composed of homogeneous particles with smooth surfaces and uniform elemental distribution (TTM), while some heterogeneous particles exhibit lamellar TTH phases precipitated on a TTM substrate.

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Conclusion

  • 章节

  • 发表日期：

    2025年

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  • Zhenyang Wang,
  • Lei Zhang,
  • Jianliang Zhang

摘要

The ironsands studied in this work primarily consist of titanomagnetite (TTM, Fe3−xTixO4) and titanomagnetite-hematite (TTH, Fe2−yTiyO3) as the dominant mineral phases. The ironsands are largely composed of homogeneous particles with smooth surfaces and uniform elemental distribution (TTM), while some heterogeneous particles exhibit lamellar TTH phases precipitated on a TTM substrate.