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Updated: Jul 9, 2026

Atom Probe Tomography Analysis of Exsolved Mineral Phases
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Published on: October 25, 2019

マントルの液体の流動は,柔らかい下層地殻を通過する:ヘリウム同位体の傾向

B Mack Kennedy1, Matthijs C van Soest

  • 1Center for Isotope Geochemistry, Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA. bmkennedy@lbl.gov

Science (New York, N.Y.)
|December 1, 2007
PubMed
まとめ

マントルの液体は,地殻の変形によって引き起こされる浸透性が向上することで,浅い地殻に到達することができます. このプロセスは,ヘリウム同位体比によって示され,潜在的な地熱エネルギー資源を強調します.

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