确定天然石英晶体的相对增长速度
1Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06520-8109, USA. phil.ihinger@yale.edu
Nature
|April 29, 2000
概括
研究人员使用微红外光谱学来分析石英晶体的生长. 杂质作为测速仪,揭示了晶体面的生长速度和地质历史.
科学领域:
- 地质化学 地质化学
- 晶体学 晶体学是指结晶学.
- 材料科学 材料科学 材料科学
背景情况:
- 在地质环境中晶体生长的理论已经确立,但对自然晶体生长持续时间的定量数据很少.
- 控制单个晶体面的尺寸和形状变化的机制尚不清楚.
研究的目的:
- 在自然晶体的整个历史中量化测量活跃晶体面的尺寸,形状和相对增长率.
- 建立一种方法来确定地质环境中晶体生长的绝对时间尺度.
主要方法:
- 在一个单一的,宝石质量的石英晶体上进行了微红外光谱研究.
- 含杂质的丰度被分析为晶体面生长速度的指标 ("速度计").
主要成果:
- 该研究成功地测量了单个晶体面的尺寸,形状和相对增长率.
- 杂质度与前进的水晶面的增长率相关,并表明了其增长率.
结论:
- 开发的微红外光谱技术允许确定晶体生长史.
- 这种方法在地质学 (岩结晶,变态,地震破裂区) 和工业 (合成晶体生产) 中具有广泛的应用.
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