概括
夏威夷玄武岩中的稀土元素模式显示出不同的分组,表明分量结晶是改变其丰富性的主要过程. 这种分析有助于理解火山岩的演变.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 同位素地质化学 同位素地质化学
背景情况:
- 夏威夷群岛代表了一个关键的海洋热点火山省.
- 了解玄武岩的微量元素变化对于破译地幔过程至关重要.
- 稀土元素 (REEs) 是岩演变的敏感指标.
研究的目的:
- 为了确定夏威夷玄武岩样本中稀土元素的度.
- 为了研究 REE 丰度模式与其他地球化学/地球物理数据之间的关系.
- 为了推断出负责观察到的REE变化的岩过程.
主要方法:
- 使用中子激活分析 (NAA) 来量化REE度.
- REE数据与现有的地质和地化学数据集一起进行了分析.
- 使用统计和图形方法来比较REE模式.
主要成果:
- 在20个分析的玄武岩中,REE的丰富性模式形成了独特的,可复制的群体.
- 这些REE分组与来自其他地质证据的分类密切相关.
- 特定的REE模式表明了岩成分的显著变化.
结论:
- 断片结晶被强烈地暗示为控制这些夏威夷基岩石中REE丰度的主导机制.
- 观察到的REE模式支持在夏威夷热点地区的不同玄武岩的不同进化途径.
- 这项研究提供了关于夏威夷群岛的岩管道系统和地幔源特征的见解.
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