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Updated: Jul 10, 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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Re-Osの同位体の証拠は,マッシフ型のアノルソサイトが地殻下部から生じたことを示している

Schiellerup1, Lambert, Prestvik

  • 1Department of Geology and Mineral Resources Engineering, Norwegian University of Science and Technology, Trondheim, Norway. henrik.schiellerup@geo.ntnu.no

Nature
|June 24, 2000
PubMed
まとめ

マッシフ型のアノルソサイト,大型のプロテロゾイク期の岩性複合体で,おそらく大陸の地殻下部の融解から発生した. ノルウェーからのレニウム・オスミウム同位体データ

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