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Updated: Nov 22, 2025

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
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炭酸コンドライト隕石は,過去100万年以内に流体流出を経験しました

Simon Turner1, Lucy McGee2, Munir Humayun3,4

  • 1Department of Earth and Environmental Sciences, Macquarie University, Sydney, NSW 2109, Australia. simon.turner@mq.edu.au.

Science (New York, N.Y.)
|January 8, 2021
PubMed
まとめ

原始的な隕石は 最近の流体流動の証拠を示し,ここ数十万年の間にウランの移動を示しています. これは,彼らの親体はまだ氷を含んでいる可能性を示唆し,初期の太陽系プロセスの理解に影響を与えます.

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