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Updated: Apr 30, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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Published on: November 16, 2013

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地球の深い上層マントルの条件で水性シリケート溶融の密度

Kyoko N Matsukage1, Zhicheng Jing, Shun-ichiro Karato

  • 1Department of Environmental Sciences, Ibaraki University, Mito, Ibaraki 310-0056, Japan. kmatsu@mx.ibaraki.ac.jp

Nature
|November 25, 2005
PubMed
まとめ

水性シリケートの融解密度は410kmの深さで,元素の結合を理解するための鍵です. 水 水 水 水 水 でした.

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