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Updated: Jul 12, 2026

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下層地殻の横の同位体不連続:南極からの例

R I Kalamarides, J H Berg, R A Hank

    Science (New York, N.Y.)
    |September 4, 1987
    PubMed
    まとめ

    南極の地殻下部の粒子を調査すると,重要な構成と年齢の不連続性が明らかになる. ストロンチウムと酸素のイソトープによって特定されたこの地質学的境界線は,南極横断の山脈の下にある古代の縫合物を示す可能性があります.

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