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铁氧化:合成Ca0.15Fe0.85SiO3铁氧化的稳定性和X射线晶体学
概括
合成的氧化物 (Ca0.15Fe0.85SiO3) 模仿了月球上的氧化物. 这种合成材料在10千巴以下是不稳定的,这表明月球上的火氧铁矿已经保持了数十亿年的转移稳定.
科学领域:
- 矿物学是什么?矿物学是什么?
- 地质化学 地质化学
- 行星科学 行星科学
背景情况:
- 氧铁矿是一种新发现的矿物质,在阿波罗11号月球样本中发现.
- 合成的Ca ((0.15) Fe ((0.85) SiO ((3) 铁氧化物与铁氧化物具有结构和组成的相似之处.
研究的目的:
- 为了研究合成Ca{0.15) Fe{0.85) SiO{3} pyroxenoid 的稳定性条件.
- 为了了解阿波罗11号样本中的月球火氧矿的持久性.
主要方法:
- 在高压下合成Ca ((0.15) Fe ((0.85) SiO ((3) 氧化.
- 合成和天然样品的结构和组成分析.
主要成果:
- 合成的Ca{0.15) Fe{0.85) SiO{3) 氧化物表现出氧化的结构.
- 这种合成材料在大约10千巴以下的压力下是不稳定的.
- 月球上的火氧铁矿可能处于转移稳定的状态.
结论:
- 在月球表面条件下,铁矿的稳定性是值得怀疑的.
- 月球上的火氧铁矿可能已经存在于转移稳定的状态上数十亿年了.
- 这些发现为月球上的长期地质过程提供了洞察力.
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