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Updated: Jul 8, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

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

Published on: June 13, 2015

原始的なプラネテシマルの蓄積:エンスタチトのコンドライトから得られたHf-W同位体の証拠

Lee1, Halliday

  • 1Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-1063, USA. Institute for Isotope Geology and Mineral Resources, Department of Earth Sciences, ETH Zurich, CH-8092, Zurich, Switzerland.

Science (New York, N.Y.)
|June 2, 2000
PubMed
まとめ

かつて地球の構成要素と考えられていたエンスタタイト・コンドライトは,固有のボルンガムの同位体データを示している. これは,内部プロセスではなく,惑星の小さな衝突から,おそらく重要なボルンガムの再分配を示唆しています.

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