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Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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リングウッドライトで示された水性マントルの移行地帯は,ダイヤモンドの中に含まれています

D G Pearson1, F E Brenker2, F Nestola3

  • 1Department of Earth and Atmospheric Sciences, 1-26 Earth Sciences Building, University of Alberta, Edmonton, Alberta T6G 2E3, Canada.

Nature
|March 14, 2014
PubMed
まとめ

地球の深層マントルの移行地帯は,かなりの量の水を保持している可能性があります. 研究者らは,ブラジルのダイヤモンドで水に富んだリングウッドライトの証拠を発見し,このゾーンが局所的に水性であることを確認した.

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