まとめ
太陽系に共通するフェロマグネシウムオリビンは,連続した固体溶液ではないかもしれません. ディヴノエ隕石から採取された天然のサンプルは,低温で混ざり合いのギャップの証拠を示しています.
科学分野:
- ミネラロジーは,鉱物学です.
- 地質化学 地質化学
- 惑星科学は惑星科学である.
背景:
- フェロマグネシウムオリビンは,太陽系に広く存在する鉱物です.
- それは伝統的に連続した固体溶液として見られてきました.
- 熱力学モデルでは,低温で潜在的混合性のギャップが示唆されている.
研究 の 目的:
- フェロマグネシウムオリビンの固体溶液における混合性のギャップの存在を調査する.
- 提案された低温混合性ギャップの賛成または反対の直接的な証拠を提供するために.
主な方法:
- 天然フェロマグネシアンオリヴィンのサンプルを分析.
- オリヴィン構造内の溶解外ラメラの検査.
主要な成果:
- ディヴノエの隕石には,明確な溶解ラメラを持つフェロマグネシアンオリビンが含まれています.
- これらのラメラは,組成的に異なる相を示す.
- これは,混合性のギャップの直接的な証拠を提供します.
結論:
- この研究は,低温での鉄・マグネシウム・オリヴィン固体溶液における混合性のギャップの存在を確認した.
- この発見は,連続的な固体溶液の行動に関する長年にわたる見解に異議を唱える.
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