まとめ
微量元素のパターンは,補完的な玄武岩源を明らかにし,マントルの分化とマグマの海洋進化を示唆しています. この研究は,源地の大きさとそのマントルの分布を推定しています.
科学分野:
- 地質化学 地質化学
- ペトロロジー・ペトロロジーとは
- マントラダイナミクス マントラダイナミクス
背景:
- 大陸,海洋島,中洋のの玄武岩は,特徴的な微量元素のパターンを表しています.
- これらのパターンを理解することは,マントルの構成と進化を解読する鍵です.
研究 の 目的:
- 微量元素データを用いて,玄武岩源地域の相対的な大きさを推定する.
- 異なるマントルの貯水池を作り出した分化プロセスを解明する.
主な方法:
- 微量元素の濃度パターンの分析,様々な玄武岩の種類.
- マントルの源領域の体積と組成物のモデリング.
主要な成果:
- 補完的な微量元素のパターンは,マントルの異なる分離した源領域を示している.
- これらの源の総量は,上層マントルの大部分を占めています.
- 中洋のの玄武岩源は,エクロジット・カミュレートから進化したもので,他のものはガーネット・ペリドータイトで濃縮されている.
結論:
- 初期のマントルの分化と結晶分化により,玄武岩源地域が分離した.
- これらの発見は,マントルの異質性について,地上のマグマの海洋起源のモデルを支持する.
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