月球的clinopyroxenes:化学组成,结构状态和质地.
概括
阿波罗11号的克林皮洛克森揭示了复杂的石和石的杂交. 这些月球火素显示出初级化学变异和溶解层,表明单一的初级火素阶段.
科学领域:
- 地质地质地质地质地质地
- 矿物学是什么?矿物学是什么?
- 行星科学 行星科学
背景情况:
- 克林诺普罗素是理解火热过程的关键矿物质.
- 阿波罗11号的样本提供了关于月球岩演变的见解.
研究的目的:
- 来自阿波罗11号月球样本的clinopyroxenes的矿物学和化学特征.
- 为了研究月球环境中的火素的形成和演变.
主要方法:
- 单晶X射线 difraktion 的使用方法.
- 微型探针分析分析
- 光学显微镜是一种光学显微镜.
- 电子显微镜 (包括传输电子显微镜)
主要成果:
- 月球的clinopyroxenes主要是形形形形的杂交.
- 观测到大量的溶解层,其薄度达到了60 Å.
- 确定了主要的化学异质,其中涉及Ca,Fe,Ti,Al和Si的相互关系.
结论:
- 一个化学不均的亚酸可能是主要的氧化物阶段.
- 从这种初级石中溶解出来的石,表明了复杂的热或化学历史.
相关概念视频
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