ガラパゴス島の熱水丘:深海掘削によって明らかになった層図と化学
まとめ
ガラパゴス山脈の水熱システムは,30万年以上前のもので,マンガンが少ない堆積物を生産することから,マンガンが豊富な堆積物に制限され,時間の経過とともに強度の低下を示しています.
科学分野:
- 海洋地質学 海洋地質学
- 水熱発電システムは,水熱発電システムです.
- 地質化学 地質化学
背景:
- ガラパゴス山丘は,海底の大規模な水熱システムを表しています.
- これらの丘の進化を理解することで,長期の地質学的過程の洞察が得られます.
研究 の 目的:
- ガラパゴス島の丘の水熱システムの年齢と堆積物の組成を調べるために.
- システムの活動と支配における歴史的変化を決定する.
主な方法:
- ガラパゴス島の丘のフィールドからの堆積物核の分析.
- マンガンの含有量を決定するために堆積堆積物の地化学分析.
- 放射線年代測定法により,システムの年齢を決定する.
主要な成果:
- ガラパゴス山脈の水熱発電システムは,少なくとも30万年前のものです.
- 古い堆積物はマンガンが少なく,この地域を大きく覆っていた.
- 現在の土砂堆積地は,マンガンに富んだ露出量が限られていることが特徴です.
結論:
- 熱水発電システムは,岩を中心としたシステムから,水を中心としたシステムへと移行した.
- ガラパゴス山丘の熱水システムの強度は地質的な時間とともに減少しています.
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