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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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Low core-mantle boundary temperature inferred from the solidus of pyrolite

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

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