和证据表明,在核心-地幔界限以上的化
Claude Herzberg1, Paul D Asimow, Dmitri A Ionov
1Department of Earth and Planetary Sciences, Rutgers University, 610 Taylor Road, Piscataway, New Jersey 08854-8066, USA. herzberg@rci.rutgers.edu
Nature
|January 11, 2013
概括
玄武岩中的高-3与-4比率表明其起源来自地球深层的源头. 这种富含,较少脱气的地幔来源可能是在地球历史早期通过核心-地幔相互作用形成的.
科学领域:
- 地质化学 地质化学
- 地质物理学 地质物理学
- 行星科学 行星科学
背景情况:
- 玄武岩中的高 (3) / (4) 比通常与原始的,未含气的下层地幔来源有关.
- 这些来源可能自地球积聚以来就被隔离了,或者分布在整个地幔中.
研究的目的:
- 调查特定的玄武岩中高的 (3) He/(4) He比率的起源.
- 使用地质化学和矿物学数据来限制源的特性和位置.
主要方法:
- 从巴芬岛,西格陵兰岛,通爪高原,戈尔戈纳岛和费尔南迪纳岛 (加拉帕戈斯岛) 的岩中分析了橄类晶组成.
- 矿来源中的含量与现代中海基岩来源中的含量的比较.
- 在研究的岩中评估同位素比率 ((3) He/(4) He).
主要成果:
- 研究的岩起源于一种矿石来源,其含量比典型的中海基岩来源高约20%.
- 这些富含的来源与高的 (3) He/(4) He比率有关.
- 证据表明,这些来源是在地球早期分化过程中通过核心-地幔相互作用形成的.
结论:
- 由核心-地幔相互作用形成的,较少脱气的,富含的地幔源被提议解释高的 (3) He/(4) He比率.
- 这种原始来源很可能是由地幔羽毛采样的.
- 在核心-地幔边界压力下的分区实验可以帮助绘制该源的空间分布图.
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