マントル由来の溶融の源における再利用された地殻の量

Alexander V Sobolev1, Albrecht W Hofmann, Dmitry V Kuzmin

  • 1Max Planck Institute (MPI) for Chemistry, Post Office Box 3060, 55020 Mainz, Germany. sobolev@geokhi.ru

Science (New York, N.Y.)
|March 31, 2007
PubMed
まとめ

リサイクルされた海洋地殻 (エクロジット) はマントルの融解に大きく影響し,ハイブリッド型ピロキセナイトを生み出します. オリビンフェノクリスタ分析は,このリサイクルされた地殻の貢献を,様々な玄武岩種とコマチートで定量化します.

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