準安定条件下で形成した鉱物の微細組織と微細構造 Microtexture and Microstructure of Minerals in Metastable Phases

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Metastable phase, which has a lager value of Gibbs free energy than that of the stable phase, commonly occurs in nature against the thermodynamic regulation. Microtexture and microstructure of some metastable-phase minerals (opal-CT, marcasite and wurtzite) are studied by high-resolution transmission electron microscopy. Disordered stacking structures are commonly observed in the metastable phases. In the case of the opal-CT (Hosaka and Akase opal mines, Japan) and marcasite (Ikezuki, Japan), highly ordered domains appear around the domains with disordered stacking structure. Chocaya-Animas wurtzite crystals overgrow on the domains of disordered stackings of sphalerite and wurtzite, which were formed from ordered sphalerite.

収録刊行物

  • 日本結晶学会誌  

    日本結晶学会誌 42(2), 148-154, 2000-04-30 

    The Crystallographic Society of Japan

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各種コード

  • NII論文ID(NAID)
    10004673307
  • NII書誌ID(NCID)
    AN00188364
  • 本文言語コード
    JPN
  • 資料種別
    ART
  • ISSN
    03694585
  • NDL 記事登録ID
    5335097
  • NDL 雑誌分類
    ZM46(科学技術--地球科学--岩石・鉱物・鉱床)
  • NDL 請求記号
    Z15-138
  • データ提供元
    CJP書誌  NDL  J-STAGE 
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