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Updated: Jul 12, 2026

X-Ray Crystallography to Study the Oligomeric State Transition of the Thermotoga maritima M42 Aminopeptidase TmPep1050
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X-Ray Crystallography to Study the Oligomeric State Transition of the Thermotoga maritima M42 Aminopeptidase TmPep1050

Published on: May 13, 2020

メタミクトポリクラゼの球状再結晶化

R C Ewing

    Science (New York, N.Y.)
    |May 3, 1974
    PubMed
    まとめ

    稀土のニオビウム・タンタール・チタン酸化物であるポリクラゼ (polycrase) で発見された球石は,チタンに富んだフェルスマイトとして知られている. これらの球石は,周囲のメタミクトマトリックスと比較して,酸化カルシウムの有意な増加を示しています.

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