相关实验视频
Updated: Jul 12, 2026

08:14
Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
概括
美国西部地区的石同位素变异可能源于地污染,而不仅仅是地幔. 南加州的岩显示出这种微妙的地对海洋岛屿玄武岩般的岩的影响.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 石化学 石化学是一门学科.
背景情况:
- 美国西部新一代玄武岩的区域同位素变化通常归因于亚大陆地幔来源.
- 南加利福尼亚州的玄武岩呈现了一个独特的案例,同位素变异性与异石缺失有关.
研究的目的:
- 为了调查加利福尼亚州南部的基岩石中同位素变化的起源.
- 为了确定地污染与地幔来源在新一代玄武岩地质化学中的作用.
主要方法:
- 在玄武岩中分析 (Nd), (Sr) 和 (Pb) 的同位素组成.
- 对岩和地幔衍生异石进行地质化学分析.
- 同位素数据与海洋岛屿玄武岩 (OIB) 组成的比较.
主要成果:
- 南加州玄武岩中的同位素变异性仅限于贫岩.
- 含有石的玄武岩具有均的,类似于OIB的同位素组成.
- 地化学数据表明OIB类岩的地微妙污染.
结论:
- 地的污染,特别是地的污染,是加利福尼亚南部岩同位素特征的一个重要因素.
- 这一发现使次大陆地幔的构造学和同位素学解释之间的差异得以协调.
- 这项研究强调了识别地幔衍生的岩石中隐秘地污染的重要性.
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