概括
来自加利福尼亚州的多洛米特晶体表现出基底堆叠障碍,与理想结构不同. 这种通过电子显微镜观察到的缺陷与1958年多洛米特非静电测量模型一致.
科学领域:
- 矿物学是一门学科.
- 地质地质地质地质地质地
- 晶体学 晶体学是指结晶学.
背景情况:
- 多洛米特是一种常见的碳酸盐矿物质,经常表现出非固体质量.
- 矿物质的基础堆叠障碍会影响其结构和化学性质.
- 之前的模型,比如戈德史密斯和格拉夫 (1958年) 的模型,提出了多洛米特非固体测量的机制.
研究的目的:
- 为了研究来自Lost Burro形成的多洛石的晶体结构.
- 为了识别和描述这些多洛米特晶体中存在的任何结构缺陷.
- 将观察到的缺陷与现有的多洛米特非固体测量和形成模型联系起来.
主要方法:
- 使用传输电子显微镜 (TEM) 检查多洛米特晶体结构.
- 分析了电子衍射模式,以检测偏离理想的多洛米特结构的偏差.
- 与既有晶体学模型对多洛米特缺陷的比较.
主要成果:
- 来自诺帕山脉的多洛米特晶体显示出显著的基底堆叠障碍.
- 电子衍射模式揭示了卫星反射,表明离子和离子堆叠的偏差.
- 观察到的障碍符合Goldsmith和Graf (1958) 提出的基底缺陷模型.
结论:
- 研究的多洛米特呈现出一种被归因于基底堆叠障碍的超结构.
- 这种缺陷与解释多洛米特非基度的模型相一致.
- 这种疾病暂时与微型石灰岩形成期间的晚期代谢基因置换条件有关.
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