キュロコ型のポリメタリック硫化物の埋蔵地で,海底のシリシックのカルデラにある
1Geological Survey of Japan 1-3, Higashi-1, Tsukuba, Ibaraki 305-8567, Japan. Smithsonian Institution MRC-119, Washington, DC 20560-0119, USA. Japan Marine Science & Technology Center 2-15, Natsushima-cho, Yokosuka 237-0061, Japan. University of Tokyo.
まとめ
金と銀が豊富なKuroko型の大規模な火山性マッシブ硫化物堆積物が,Myojin Knollの海底カルデラで発見された. この発見は,未探査の海底のシリシックの caldera に同様のポリメタリック堆積物が存在する可能性があることを示唆しています.
科学分野:
- 海洋地質学 海洋地質学
- 経済地質学 経済地質学
- 火山学 火山学とは
背景:
- キュロコ型鉱床は,多金属鉱物の重要な資源である.
- 海底熱炉は,大規模な硫化物埋蔵の未熟な環境である.
研究 の 目的:
- Kuroko型の大規模な火山性マッシブ硫化物堆積物の発見を報告するために.
- 他の潜水艦の caldera で同様の堆積物の可能性を評価する.
主な方法:
- 乗組員付き潜水艦の調査が行われました.
- 地質的地図作成と硫化物堆積物のサンプル採取が行われました.
主要な成果:
- 大きく,活発に成長するKuroko型鉱床は,Myojin Knollカルデラ床 (1210~1360m深さ) で発見されました.
- 鉱床の面積は400×400×30メートルで,金と銀が豊富に含まれています.
- 鉱床は,弧面の海底カルデラの中に位置しています.
結論:
- この発見は,海底のシリシックの caldera で重要なポリメタリック硫化物埋蔵の可能性を強調しています.
- 追加の資源を特定するために,同様の環境のさらなる探査は正当化されています.
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