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Updated: May 11, 2026

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海洋地殻の流通した流体の流れは,熱流と浸透性のデータを調和させる

Fisher1, Becker

  • 1Earth Sciences Department, University of California, Santa Cruz 95064, USA. afisher@es.ucsc.edu

Nature
|January 19, 2000
PubMed
まとめ

海底地殻における熱水流体循環は,海洋と地殻の組成に不可欠である. 地域の浸透性は,掘削穴のデータが示唆するよりも高く,古い海洋地殻の流れがチャネル化されていることを示しています.

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