相关实验视频
Updated: Jun 29, 2026

04:36
Production of Synthetic Nuclear Melt Glass
Published on: January 4, 2016
融化产量低于Mt. 沙斯塔从原始融体内含的数据中得出
概括
在山上的同位素. 沙斯塔岩表明,沉降板块的脱水导致了岩的产生. 这挑战了主导理论的地幔子融仅仅由流体.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 石化学 石化学是一门学科.
背景情况:
- 弧形岩通常由由于板块流体而导致的地幔融形成.
- 海洋地,特别是年轻而热的石化层,也可能有助于弧形岩的产生.
研究的目的:
- 调查基岩岩石岩岩在山上的起源. 沙斯塔. 沙斯塔. 这就是沙斯塔.
- 确定浮板材料在岩生成中的作用.
主要方法:
- 在位测量同位素组成 (delta(11) B) 在含有橄素的融物中.
- 在原始融中含量的分析.
主要成果:
- 在山上的同位素. 沙斯塔的样本显示出很大的负值和变量值 (delta) 11B = -21.3到-0.9每毫米).
- 的度相对较低 (0.71.6 ppm).
- 观察到度和同位素组成之间的相关性.
结论:
- 观察到的同位素特征支持了脱水降压板材对Mt. 沙斯塔的玄武岩石岩石是一种岩石岩石.
- 这一发现提供了证据,证明地对弧形岩形成的贡献.
- 这项研究强调了分析融化含物的重要性,以了解岩源.
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