オスミウムイソトープの制約により,鉱石の金属リサイクルが潜水地帯で制限されます
1Commonwealth Scientific and Industrial Research Organization Exploration and Mining, Post Office Box 136, North Ryde, New South Wales 1670, Australia; Department of Earth Sciences, Monash University, Clayton, Victoria 3168, Australia;
まとめ
ラドラム金鉱の下にある有線マントル岩は,高濃度の銅,金,プラチナ,パラジウムを含んでいる. これらの金属は,おそらくマントルから発生し,テクトニックプロセスによって濃縮された.
科学分野:
- 地質化学 地質化学
- 経済地質学 経済地質学
- マントル・ペトロロジー マントル・ペトロロジー
背景:
- 静脈状のペリドータイト・キセノライトは,パプアニューギニアのリヒル島にあるラドラム金鉱の下のマントルで見つかりました.
- これらのクセノライトは,周囲の枯渇した弧のマントルと比較して,銅,金,プラチナ,パラジアムの濃度が大幅に高くなります.
研究 の 目的:
- ラドラム金鉱の金属の起源を調査する.
- ポルフィール-エピテルマルの銅-金鉱床の形成におけるマントルの役割を理解する.
主な方法:
- ペリドータイト・キセノリスの主要元素と微量元素の分析.
- 金鉱石とマントルのペリドータイトのオスミウム同位体分析.
主要な成果:
- ペリドライト・キセノライトは,周囲のマントルと比較して,Cu,Au,Pt,Pdで2~800倍濃縮されている.
- 金鉱石のオスミウムイソトープ組成は,潜水改変マントルのペリドータイト源と一致する.
- マントルは,ラドラム鉱床の金属の主要な供給源である.
結論:
- マントルは,ラドラム金鉱の金属の主要な供給源である.
- 液体溶性金属を濃縮する地質学過程は,ポルフィール-エピテルマルの銅-金堆積物の形成に不可欠である.
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