概括
在高压 (56 GPa) 下,石的冲击变形产生了第一个观察到的橄玻璃. 这一发现表明,50-55 GPa以上的冲击事件可以在天然橄中形成玻璃.
科学领域:
- 地质地质地质地质地质地
- 材料科学 材料科学 材料科学
- 矿物物理 矿物物理
背景情况:
- 石是矿物奥利文的宝石质量品种,是地球上层地幔的主要组成部分.
- 了解橄在极端条件下的行为对于行星科学和地质物理学至关重要.
研究的目的:
- 为了研究经过实验冲击变形的自然岩中的微观结构变化.
- 为了确定任何由冲击产生的无形相的形成条件和特征.
主要方法:
- 使用传输电子显微镜 (TEM) 检查了一颗自然晶的单晶.
- 经过实验,透物样本经过冲击变形,达到大约56 GPa的峰值压力.
主要成果:
- 观察到的无形区域,被认定为橄玻璃,在受冲击的周围物体的晶体区域内.
- 玻璃形成与表现出高密度的纠突变区域密切相关.
- 该研究提供了首次报告的冲击诱导的橄玻璃观察.
结论:
- 橄玻璃可能在自然橄中形成,其冲击压力大约超过50-55GPa.
- 对自然冲击的橄树进行进一步的TEM研究可以证实冲击诱导的玻璃的广泛存在.
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