一些羽毛中的-187丰富:证据表明核心-地幔相互作用?
概括
地球外核的/和-187/-188比重可能高于状上层地幔. 这种同位素特征起源于核心-地幔边界,可以在地幔羽毛中检测到.
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:
- 地球的核心-地幔边界 (D"层) 是理解行星分化的一个关键区域.
- 诸如的元素的同位素比率为地质过程提供了关键的标志物.
研究的目的:
- 为了研究地球外核的潜在同位素组成.
- 为了确定在地幔羽毛中是否可以检测到核心材料.
主要方法:
- 使用基于小行星核心数据的计算.
- 分析/和-187/-188的比例.
主要成果:
- 地球外核的/比可能至少比状上层地幔高20%以上.
- 外部核心的-187/-188比率可能至少比丁石高8%.
- 羽毛衍生系统中同位素的丰富度 (比地质高5-20%) 与核心-地幔边界源相一致.
结论:
- 外部核心很可能与状地幔相比,富含和.
- 地幔羽毛可以携带核心-地幔边界的同位素特征.
- 这提供了核心和地幔之间物质交换的证据.
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