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Updated: Jul 11, 2026

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Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
まとめ
原始ヘリウムは,海洋と大陸の両方の地殻を通って地球のマントルから脱出し,亜大陸の脱ガス化は,活発な地殻の拡張に関連しています. このプロセスは,地球の熱とヘリウムバランスの現在のモデルに挑戦しています.
科学分野:
- 地質化学 地質化学
- 地質物理学 地質物理学とは地質物理学です.
- 地球科学 地球科学 地球科学
背景:
- 地球の形成以来閉じ込められた原始のヘリウムは,新しい海殻を通して脱ガスされます.
- 予想とは対照的に,大陸の地殻を通って重要なヘリウム脱ガスも発生しています.
研究 の 目的:
- ヘリウムの脱ガス化という,ほとんど理解されていない亜大陸のプロセスを調査するために.
- マントルの熱損失とヘリウム損失の観測速度を調和させるため.
主な方法:
- マントルの揮発性物質が大陸の地殻,特に西ヨーロッパから脱出する分析.
- ヘリウム損失率と,ウランとソリウムからの放射性熱生成の比較.
主要な成果:
- 西ヨーロッパにおけるマントルの揮発性脱出は,活発な地殻拡張と関連しています.
- マントルの熱失失の現在の速度は,ヘリウム失失の速さ (~20の因数) よりも著しく高い.
結論:
- サブコンチネンタルヘリウム脱ガス化は,地殻が活発に拡張している場所で発生する重要なプロセスです.
- 熱とヘリウム損失率の不一致は,マントルにヘリウムが蓄積されているか,地球の大量化学と熱源のモデルに誤りがあることを示唆しています.
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