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Updated: Jun 17, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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Published on: November 15, 2013

地球のマントルにある隕石Krは,大気圏の後期的な増積源を示唆している

Greg Holland1, Martin Cassidy, Chris J Ballentine

  • 1School of Earth, Atmospheric, and Environmental Sciences, University of Manchester, Oxford Road, Manchester M13 9PL, UK. g.holland@manchester.ac.uk

Science (New York, N.Y.)
|December 17, 2009
PubMed
まとめ

地球のマントルに発見された原始的なクリプトン (Kr) は,流星石や初期の太陽星雲から発生した揮発性物質を示唆しています. 地球の大気と海洋は,初期の放気ではなく,後の揮発性捕獲から高貴ガスを獲得した可能性が高い.

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