アラビアのアル・ハディダ近郊のワバルクレーターからのコエサイト
まとめ
高圧のシリカポリモルフであるコエサイトは,アラビアのワバル隕石クレーターで発見された. これは3つの衝突クレーターの中で最小のクレーターで見つかったコエサイトの3番目の自然発生です.
科学分野:
- ミネラロジーは,鉱物学です.
- 地質学 地質学 地質学
- インパクトクレーター研究
背景:
- コエサイトは,シリカの高圧ポリモルフである.
- コエサイトの自然発生は稀であり,重要な地質学的発見である.
- 隕石のクレーターは,激しい圧力と温度がある場所であり,潜在的に高圧鉱物を形成します.
研究 の 目的:
- 第3回自然発生のコエサイトを報告する.
- ワバル隕石クレーターで発見されたコエサイトを記録するために.
主な方法:
- ワバル隕石クレーターの地質調査.
- コエサイトを特定するための鉱物学的分析.
主要な成果:
- コエサイトは,アラビアのワバル隕石クレーターで確認された.
- ワバルクレーターは直径約300フィート,深さ40フィート.
- この発見は,コエサイトを含む3つの既知のクレーターの中で最小のクレーターを表しています.
結論:
- ワバル隕石クレーターは,高圧鉱物形成を理解するための重要な場所です.
- ワバルでのコエサイトの存在は,独特の地質学的条件を作り出す衝撃イベントのさらなる証拠を提供します.
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