ウィドマンスタッテンのパターンは,金属を含有する陸上の岩石であるジョセフィナイトにある
まとめ
ゆっくりとした冷却による溶解構造であるウィドマンスタッテンパターンは,陸上の岩であるジョゼフィナイトで発見されました. この発見は,ジョセフィナイトが地球のマントルから生まれたことを示唆しています.
科学分野:
- 地質学 地質学 地質学
- ミネラロジーは,鉱物学です.
- ペトロロジー・ペトロロジーとは
背景:
- ジョゼフィナイトは,蛇形化したペリドータイトのプレッシャーに含まれるユニークな金属性岩です.
- 陸上の岩は通常,Widmanstaettenパターンを表さない.
研究 の 目的:
- ジョゼフィナイト標本におけるウィドマンスタッテンパターンの存在と起源を調査する.
- ジョゼフィナイトの熱的経歴と源を決定するために.
主な方法:
- オレゴン州南西部のジョセフィナイト標本の顕微鏡検査.
- 金属相組成と溶解質感の分析.
主要な成果:
- 緩やかな冷却による溶解の特徴であるWidmanstaettenパターンは,変化が少ないジョゼフィニット領域で特定されました.
- 大量組成は,最初の均質な金属が500°C以上存在していたことを示している.
- これらのパターンは,既知の地上の岩石に前例のないものです.
結論:
- 観測されたWidmanstaettenパターンは,ジョゼフィナイトのマントルの起源の強力な証拠を提供します.
- ジョゼフィナイトの熱の歴史は,高温の源からゆっくりと冷却されることで一致しています.
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