多色极化:提高了古老的古老的石墨显微镜的功能
Bernardo Cesare1, Nicola Campomenosi2,3, Michael Shribak4
1Department of Geosciences, University of Padova, via G. Gradenigo 6, 35131 Padua, Italy.
概括
多色极化显微镜 (PPM) 揭示了像石榴石这样的低断材料中微妙的微观结构. 这种新的光学技术为地质材料分析提供了一个快速,丰富多彩和非破坏性的替代方案.
科学领域:
- 地质地质地质地质地质地
- 光学显微镜的使用方法
- 材料科学 材料科学 材料科学
背景情况:
- 传统的偏振显微镜与具有较低双折射率 (1-300 nm阻抗) 的材料进行斗争.
- 像石榴石这样的矿物质中微妙的微观结构,由生长或应变引起,通常无法用标准方法检测到.
研究的目的:
- 介绍和演示多色极化显微镜 (PPM) 的应用,用于分析地质材料.
- 突出PPM在低折射率样本中可视化微结构的能力,特别是石榴石.
主要方法:
- 多色极化显微镜 (PPM) 应用于30微米岩石薄片.
- 分析石榴石中微妙的双折射,考虑非同位素生长和应变诱导的影响.
主要成果:
- PPM产生了全谱彩色图像,揭示了在传统显微镜下看不见的微观结构.
- 该技术有效地可视化了石榴石中微妙的双断裂,与生长和压力有关.
结论:
- PPM是一种强大的新光学技术,用于对地质材料的微结构分析.
- 它为基于SEM的方法提供了一个快速,非破坏性的和具有成本效益的替代方案,用于初始微观结构评估和目标识别.
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