3万年の水熱活動が失われた街の換気場にある
Gretchen L Früh-Green1, Deborah S Kelley, Stefano M Bernasconi
1Department of Earth Sciences, Eidgenössische Technische Hochschule, Zürich (ETH-Z), CH-8092 Zurich, Switzerland. gretli@erdw.ethz.ch
まとめ
ロスト・シティの水熱活動は,蛇形化によって引き起こされ,3万年以上続いている. この地質学的プロセスは,海水がペリドート岩と相互作用することで,潜在的に何百万年もの間,このようなシステムを維持することができます.
科学分野:
- 地質化学 地質化学
- 地質学 地質学 地質学
- 海洋学 海洋学とは
背景:
- ロストシティ水熱場はオフアックスシステムです.
- 蛇形化は,海水とペリドート岩の反応を伴う重要な地質学的プロセスです.
研究 の 目的:
- ロスト・シティの熱水活動期間と速度を記録する.
- 長期的な熱水システムを維持するメカニズムを理解する.
主な方法:
- ストロンチウム,炭素,酸素の同位体分析.
- 放射性炭素年代測定法 放射性炭素年代測定法
主要な成果:
- 少なくとも3万年もの間,水熱活動があった証拠があります.
- 蛇形化率は年間1.2×10−4立方キロメートルと推定されている.
- 決定的な要因を特定した:海水によるペリドート岩へのアクセス,断層,膨張,質量損失.
結論:
- 蛇形化は,ロスト・シティの水熱活動の長期的原動力である.
- これらのシステムは,数十万年から数百万年持続することができます.
- この発見は,ゆっくりと超ゆっくりと広がる環境における類似のシステムを理解するために重要である.
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