最高的陆地恒星从核心可信
F Horton1, P D Asimow2, K A Farley2
1Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA. fhorton@whoi.edu.
Nature
|October 18, 2023
概括
科学家在巴芬岛的岩中发现了异常高的-3 (3He) 与-4 (4He) 的比率,这表明了这种原始气体的潜在核心起源. 这一发现挑战了长期以来关于的观点
科学领域:
- 地质化学
- 地质学
- 地球科学
背景情况:
- 覆盖层岩通常比上层覆盖层具有更高的3He/4He比率.
- 高的3He/4He比率传统上归因于太阳星云中的原始物质在地球积聚过程中被纳入.
- 这种成分被认为在地幔中保持孤立,避免脱气事件.
研究的目的:
- 在陆地岩石中研究异常高的3He/4He比率的起源.
- 测试地球核心可能是原始的来源的假设.
- 重新评估地球内部挥发性元素的演变模型.
主要方法:
- 在巴芬岛的晶体中分析同位素比率 (3He/4He).
- 地质化学和地质物理建模以评估潜在的来源.
主要成果:
- 在陆地岩石中测定了有史以来最高的3He/4He比率 (67.2±1.8倍大气比率).
- 在巴芬岛的岩中观察到的比例与地球核心的潜在贡献一致.
- 这一发现挑战了原始在地球上的位置和生存的既定理解.
结论:
- 地球的核心可能是某些地幔岩层中观察到的高3He/4He的可行来源.
- 这种高比例的存在挑战了长期以来的假设,即原始挥发物只能在地幔中生存.
- 这一发现需要对地球深层的挥发性库存及其演变的模型进行修订.
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