在月球上进行矿物学和岩石学研究的Anorthosite幻灯片15415,1818
概括
这项研究分析了15415,18号石岩,揭示了其构成的青酸盐和火素的成分. 这些发现表明,在深层地的环境中,来自特定类型的岩的藻类生长的形成.
科学领域:
- 地质地质地质地质地质地
- 石化学 石化学是一门学科.
- 矿物学是什么?矿物学是什么?
背景情况:
- 石岩是理解行星地形成的关键.
- 了解anorthosites的石化过程,可以了解早期的岩过程.
研究的目的:
- 为了表征15415,18.18的anorthosite样本的矿物学和纹理特征.
- 为了确定这个异构体的石化条件和岩源.
主要方法:
- 薄切口的石化分析. 薄切口的石化分析.
- 电子微探测分析用于矿物成分的确定.
主要成果:
- 样本15415,18主要是青酸 (98%),含有高酸 (97%mol%).
- 两种火素,二氧化和高,存在于间歇性和作为包含在塑类中.
- 矿物质质地质和成分表明,从加布罗亚性无石岩中形成的积成长的质.
结论:
- 石可能是在一个浮动的环境中形成的.
- 这些数据支持了从超性或加布罗性无岩岩中积聚质的模型.
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