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Updated: Jun 25, 2026

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
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異常な金属に富んだ液体は,水熱鉱石の鉱床を形成する

Jamie J Wilkinson1, Barry Stoffell, Clara C Wilkinson

  • 1Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, Exhibition Road, London SW7 2AZ, UK. j.wilkinson@imperial.ac.uk

Science (New York, N.Y.)
|February 7, 2009
PubMed
まとめ

水熱鉱石の鉱床は,金属に富んだ液体から形成されます. スファレライトの液体インクルージョンを分析すると,以前に理解されていたよりもはるかに高い金属濃度が明らかになり,鉱石形成の既存のモデルに挑戦しました.

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