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Updated: Jun 18, 2026

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
09:45

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

Published on: July 24, 2016

大陸の地殻下部の原産鉄:石油学および地質学的な影響

S E Haggerty, P B Toft

    Science (New York, N.Y.)
    |August 16, 1985
    PubMed
    まとめ

    地殻下部のキセノリトで発見された原生鉄 (Fe(0) は,地球の深い地殻の環境が減少したことを示唆しています. この発見は,石層から発生する磁気異常の解釈に影響を与えます.

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