相关实验视频
Updated: Jul 7, 2026

08:14
Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
概括
高10和的度表明压板的贡献. 新的数据表明,板材材料是均的,不储存在地幔中,调节了探区的岩生成.
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:
- 引板是弧形岩来源的关键贡献者.
- 从潜水板到弧形岩源的物质转移的确切机制仍在争论中.
- 10和同位素的比率是潜伏贡献的关键标志物.
研究的目的:
- 为了研究从潜流板转移到弧形岩源的物质转移过程.
- 评估不同弧度的板块贡献的组成均性.
- 为了确定地幔内沉降的命运.
主要方法:
- 在弧形岩石中分析10/ (10Be/Be) 的比率.
- 在弧形岩石中分析/ (B/Be) 的比率.
- 在四个不同的俯冲区进行比较研究.
主要成果:
- 石块衍生材料的贡献在每一个研究的弧度内都在组成上是均的.
- 沉降似乎没有被储存在亚弧地幔中.
- (10) Be/Be 和 B/Be 数据提供了一个一致的俯冲影响图.
结论:
- 材料从潜流板转移到弧形岩源是一个规范良好的过程.
- 沉降被有效地纳入弧形岩,而不是在地幔中积累.
- 像10Be和B这样的同位素痕迹证实了潜水和弧形岩之间存在直接和均的联系.
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