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Updated: May 3, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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ピロライトの固体から推論されたコアとマントルの境界の低い温度

Ryuichi Nomura1, Kei Hirose, Kentaro Uesugi

  • 1Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551, Japan.

Science (New York, N.Y.)
|January 18, 2014
PubMed
まとめ

地球のマントル固体温は,コアマントル境界付近で驚くほど低い. この発見は,コア-マントルの境界温度の上限を設定し,地球深層のプロセスに関する私たちの理解に影響を与えます.

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