在奥利文中的溶解度以及海洋岛屿玄武岩中高3He/4He的含量
Stephen W Parman1, Mark D Kurz, Stanley R Hart
1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Building 54, Cambridge, Massachusetts 02139, USA. stephen.parman@durham.ac.uk
Nature
|October 21, 2005
概括
海洋岛屿玄武岩中的高-3/-4比率暗示了一个未含气的地幔. 新的实验表明,在地幔化过程中比和更兼容,在耗尽的残留物中保持这些比率.
科学领域:
- 地质化学 地质化学
- 同位素地球化学 同位素地球化学
- 石化学 石化学是一门学科.
背景情况:
- 海洋岛基岩 (OIB) 中高的3He/4He比率是未有气体的地幔储库的关键证据.
- 地幔融模型依赖于的化学行为,但分区估计冲突.
研究的目的:
- 为了实验性地确定在olivine中的可溶性.
- 为了澄清地幔融化过程中的分离行为.
主要方法:
- 在大气压下实验测量天然和合成橄中的可溶性.
- 与气氛平衡,然后进行粉碎和融化分析.
主要成果:
- 确定了的奥利文融分区系数,范围从0.0025 ± 0.0005到0.0060 ± 0.0007.
- 在地幔融化过程中,似乎比和更兼容.
结论:
- 实验数据表明在化过程中的兼容性,可能在耗尽的残留物中保持高的3He/4He比率.
- 这解决了OIB和中海基岩度之间的差异,支持高3He/4HeOIB的耗尽来源.
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