相关实验视频
Updated: Jul 15, 2026

11:32
High Pressure Single Crystal Diffraction at PX^2
Published on: January 16, 2017
天然NaAlSi(3)O(8) - - 荷兰石在被冲击的西考石中的发现
1Laboratoire de Sciences de la Terre, Ecole Normale Superieure de Lyon et Universite Claude Bernard Lyon I (UMR CNRS 5570), 46, allee d'Italie, 69364 Lyon Cedex, France. Max-Planck-Institut fur Chemie, Joachim-Becher-Weg 27, D-55128 Mainz,
概括
在受冲击的石静脉中发现了Hollandite高压多态质. 这一发现为在小行星撞击中经历的极端压力提供了新的见解.
科学领域:
- 矿物学是什么?矿物学是什么?
- 行星科学 行星科学
- 地质化学 地质化学
背景情况:
- 木是一种在陆地和外星岩石中常见的矿物.
- 冲击事件可以诱导矿物质中的高压多态.
- 之前的研究在冲击石中发现了maskelynite,但其确切的矿物质被争论.
研究的目的:
- 为了识别和表征在Sixiangkou L6合体中的压力高的多态合体.
- 为了确定这种多态的晶体学性质和单元细胞参数.
- 使用矿物质组合来限制冲击事件期间的峰值压力.
主要方法:
- 激光微拉曼光谱分析矿物质的组成和结构.
- 通过X射线衍射来确定晶体学参数.
- 在西山口L6石中,对冲击诱导的融化静脉的岩石分析分析.
主要成果:
- 标识了Hollandite的高压多态形态的Plagioclase.
- 这种矿物质与前maskelynite颗粒中的田地玻璃交织在一起.
- 用单元格参数 a = 9.263 ± 0.003 Å 和 c = 2.706 ± 0.003 Å 确定四角形结构.
- 同时发生在多数酸铁烯固体溶液和酸盐中.
结论:
- 荷兰的存在提供了直接的证据,证明在冲击条件下,高压转化形成了质.
- 相关的矿物质组合限制了融化静脉中的峰值冲击压力.
- 没有铁结构相表明结晶压力低于大约23千兆帕斯卡尔.
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