Science (New York, N.Y.)
|January 9, 1970
PubMed
まとめ

研究者らは,南極の海氷の下に形成されたユニークな氷のステラクティスを発見しました. これらの空洞で円筒状の構造は,氷床から海に流れる濃厚で冷たい塩水によるものです.

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