相关实验视频
Updated: Jul 12, 2026

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Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
概括
ортопироксен片通过两步的过程从石中生长:扩散和克利诺海珀斯逆转. 这种机制解释了 orthopyroxene 形成与clinohypersthene 边缘,由元素梯度分析支持.
科学领域:
- 矿物学是什么?矿物学是什么?
- 地质化学 地质化学
- 晶体学 晶体学是指结晶学.
背景情况:
- 奥吉特是一种富含的氧化,通常含有溶解的正氧化片.
- 精确的机制的骨皮洛克森叶片生长在奥吉特一直是正在进行的研究的主题.
研究的目的:
- 为了阐明从石中溶解出来的整形皮洛克森叶片的生长机制.
- 为了研究扩散和相变的作用在叶片形成.
主要方法:
- 使用电子微探针分析等技术,分析层接口上的元素度梯度.
- 微观结构检查溶解的片,以确定结晶学特征.
主要成果:
- ортопироксен板的生长通过两步过程发生: (i) 和 (,铁) 的扩散形成克利诺,以及 (ii) 克利诺的反转成 ортопироксен.
- 由于冷却或度梯度的不完全反转,导致有clinohypersthene边缘的orthopyroxene.
- 在100个接口处测量到的元素度梯度支持了拟议的两步增长机制.
结论:
- 从石中脱离正氧化是一种复杂的过程,涉及扩散和固态反转.
- 临高边缘的存在是叶片生长过程中不完全逆转的直接后果.
- 这项研究提供了一个详细的机械的理解的pyroxene exsolution现象.
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