相关实验视频
Updated: Jun 25, 2026

11:32
High Pressure Single Crystal Diffraction at PX^2
Published on: January 16, 2017
在alpe arami peridotite中的clinoenstatite:额外证据表明非常高的压力
Bozhilov1, Green, Dobrzhinetskaya
1Institute of Geophysics and Planetary Physics and Department of Earth Sciences, University of California, Riverside, CA 92521, USA.
概括
传输电子显微镜揭示了在瑞士阿尔卑斯山石榴石 (lherzolite) 中的克里诺恩斯塔提特片. 这些发现表明,大陆碰撞前至少250公里的深层岩石被挖掘出来.
科学领域:
- 矿物学和石器学 矿物学和石器学
- 地质化学 地质化学
- 构造学 构造学 构造学 构造学
背景情况:
- 石榴石lherzolites提供了关于地球上层地幔的组成和条件的见解.
- 了解矿物质溶解板块有助于重建地质历史.
- 阿尔佩阿拉米山脉是研究地幔外层岩石的关键地点.
研究的目的:
- 为了研究二氧化物颗粒内部的克里诺恩斯塔提特片的微观结构和晶体学.
- 解释溶解过程并推断宿主岩石的P-T条件.
- 为了确定阿尔佩阿拉米石榴石 (lherzolite) 的挖掘深度.
主要方法:
- 传输电子显微镜 (TEM) 用于矿物微结构的高分辨率成像.
- 溶解后的晶体分析.
- 在二氧化-克利诺恩斯塔提特系统中的相位关系分析.
主要成果:
- 在Alpe Arami石榴石lherzolite的二氧化物颗粒中发现了克利诺恩斯塔提特的斑块.
- 导向,晶体学和微观结构与从高压C中心的克里诺恩斯塔提特相中脱离的溶液一致.
- 阶段关系的分析支持了这一解释.
结论:
- 在C中心的克利诺恩斯塔提特的脱离表明在高压下形成.
- 这些叶片的存在意味着这些岩石从至少250公里的深度被挖掘出来.
- 这次挖掘事件可能发生在大陆碰撞之前或期间.
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