概括
斯蒂索维特的晶体形状随着高压的结晶温度而变化. 这一发现可能有助于确定撞击坑的高峰温度,这表明流星坑经历了超过900摄氏度.
科学领域:
- 矿物学是一门学科.
- 地质化学 地质化学
- 行星科学 行星科学
背景情况:
- 斯蒂索维特是二氧化的高压多态,表现出明显的结晶习惯.
- 了解这些习惯对于解释地质条件至关重要.
研究的目的:
- 为了研究stishovite晶体习惯和高压结晶温度之间的关系.
- 为了评估stishovite作为撞击事件的地质温度计的潜力.
主要方法:
- 在约120千巴的stishovite的结晶实验中.
- 在不同温度条件下对晶体形态的微观分析.
主要成果:
- 在低于600°C的温度下,石形成双金字塔状晶体.
- 在600°C和900°C之间,可以观察到颗粒状晶体.
- 在900°C以上,会形成针状晶体.
结论:
- 斯蒂索维特的取决于温度的结晶习惯可以作为高压地质温度计.
- 在石坑中发现的Acicular stishovite表明结晶温度超过900°C.
- 这对了解撞击地点的热条件有影响.
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