まとめ
カルカ・イントルーションは複雑なオープンシステムの振る舞いを示し,同位体データは大規模な国土岩の汚染と変数マグマ組成を明らかにし,層状の侵入に対する単純な分量結晶化モデルに挑戦しています.
科学分野:
- 地質学
- 地化学
- ペトロロジー
背景:
- オーストラリア中部のジャイルズ・コンプレックスの一部であるカルカ・イントルーションは,ピロクセナイトからアノルトサイトまでの層状の層構造を示しています.
- その21の周期単位は分数結晶化を示唆しますが,同位体データはより複雑なプロセスを示しています.
研究 の 目的:
- カルカ侵入のマグマプロセスと汚染の歴史を調査する.
- マフィー・ウルトラマフィー・侵入の 伝統的な解釈に挑戦する
主な方法:
- 初期ストロンチウム (Sr) とネオジミウム (Nd) の同位体の比率の分析
- ミネラル結晶の配列と組成の変化の調査.
主要な成果:
- 初期の87Sr/86Sr比と通常の143Nd/144Nd比は,カントリー・ロックに重大な汚染があることを示している.
- Sr初期比 (0.70490.7088) の広い範囲は,分断を超えた変数マグマ組成を示唆している.
結論:
- カルカ・イントルーションは 単純な断片結晶化ではなく 複雑なオープンシステムで形成された
- アイソトップの異質性は,大規模な汚染と/または様々なマグマバッチの配置を示しています.
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