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Updated: Jul 12, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

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オスミウム187の濃縮は,いくつかの羽根で:コア-マントルの相互作用の証拠?

R J Walker, J W Morgan, M F Horan

    Science (New York, N.Y.)
    |August 11, 1995
    PubMed
    まとめ

    地球の外核は,コンドリート上のマントルよりも高いレニウム/オスミウムとオスミウム187/オスミウム188の比率を有している可能性があります. この同位体シグネチャーは,コアマントルの境界から発生し,マントルの羽根で検出できます.

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