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Updated: May 26, 2025

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颗粒边界扩散不能解释深层地幔的W同位素异质性

Yihang Peng1, Takashi Yoshino2, Jie Deng3

  • 1Department of Geosciences, Princeton University, Princeton, NJ, USA. yhpeng@princeton.edu.

Nature communications
|February 21, 2025
PubMed
概括

来自地球核心的 (W) 扩散不太可能解释海洋岛基岩中的同位素变异. 分子动力学模拟表明,W扩散在核心-地幔边界太慢,无法影响岩石中的W同位素.

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