銅がマグマ質の蒸気相へと極端に分割される証拠がある
まとめ
火山ガスバブルに含まれる硫化銅は,浅いマグマ室内の蒸気に銅が濃縮されていることを示している. この発見は,大気への金属の貢献と銅鉱石埋蔵の形成を理解するために極めて重要です.
科学分野:
- 地質化学 地質化学
- 火山学 火山学とは
- 経済地質学 経済地質学
背景:
- マグマ室は,多様な地質学的過程を宿している.
- マグマティック・システムにおける金属の振る舞いを理解することは,資源探査の鍵です.
- 大気中の金属に起因する火山の貢献は大きい.
研究 の 目的:
- 浅いマグマ室に銅が存在する段階を調査する.
- 磁気蒸気と溶融の間の銅濃度差を定量化するために.
- 銅の揮発性行動が,大気中の金属循環と鉱石堆積の形成に及ぼす影響を評価する.
主な方法:
- フェノクリストに宿る溶融インクルージョンの分析.
- ガス泡の中の硫化銅の識別.
- 蒸気と融解相の化学分析.
主要な成果:
- 二酸化炭素と塩素を含むバブルで発見された硫化銅.
- 銅は,浅いマグマ室内の蒸気相に濃縮されています.
- マグマ蒸気は,同時に存在するパンテレライト溶融よりも数百倍の銅濃度を示しています.
結論:
- 磁気蒸気中の銅の存在は,特定の浅い磁気系で確認されています.
- 銅の揮発性行動は,大気中の金属モデリングにおける重要な要因です.
- この振る舞いは,銅のポルフィール鉱石の鉱床の発生に重要な役割を果たす可能性があります.
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