微量元素在深层岩海洋中的分割和Hf-Nd地幔阵列阵列的起源
Keisuke Ozawa1, Naoya Sakamoto2, Yutaro Tsutsumi1
1Department of Earth and Planetary Science, The University of Tokyo, Tokyo 113-0033, Japan.
Science advances
|August 16, 2024
概括
地球深处的结晶分成微量元素,影响地幔同位素. 实验显示,桥石/融分区系数随着压力显著变化,影响了下层地幔的Lu/Hf和Sm/Nd比率.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 行星科学 行星科学
背景情况:
- 岩海洋结晶可能会分解微量元素,影响下层地幔的同位素组成.
- 之前关于微量元素分割的实验数据仅限于上下地幔压力.
研究的目的:
- 为了确定La,Nd,Sm,Lu和Hf的桥/化分区系数 (D).
- 为了覆盖地球整个下层地幔 (24至115GPa) 的压力范围.
主要方法:
- 高压实验模拟了地幔下层条件.
- 测量了布里格曼石和化石之间的微量元素分区.
- 在广泛的压力范围内分析分区系数 (D).
主要成果:
- 观察到D_Lu和D_Hf的显著减少,压力增加至91GPa.
- 在深下地幔条件下,D_Lu/D_Hf > 1 和 D_Sm/D_Nd < 1 .
- 布里奇曼石结晶的演变融化向低的Lu/Hf和高的Sm/Nd比率.
结论:
- 低地幔深层结晶驱动了显著的微量元素分化.
- 这个过程可以解释地球地幔的同位素组成.
- 建议在最下层地幔中隐藏一个残余化的隐藏储存库.
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