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Updated: Jul 11, 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

現代の弧における古代のマントル: izu-bonin-mariana forearcにおけるオスミウム同位体,peridotitesにおけるオスミウム同位体

Parkinson1, Hawkesworth, Cohen

  • 1Department of Earth Sciences, Open University, Walton Hall, Milton Keynes MK7 6AA, UK.

Science (New York, N.Y.)
|September 25, 1998
PubMed
まとめ

イズー・ボニン・マリアナ前弓のマントル・ペリドータイトにおけるオスミウム同位体は,古代の枯渇現象を明らかにしている. これらの発見は,サブドクションゾーンが,マントルの初期の融解の証拠を保存している可能性を示唆し,コンベクトの上層マントルの私たちの理解に影響を与えます.

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