概括
阿波罗11号的月球岩石经历了微弱到中度的冲击事件. 矿物碎片的分析揭示了微观结构效应和冲击诱导的化,表明压力约为100-200千巴.
科学领域:
- 地质地质地质地质地质地
- 行星科学 行星科学
- 矿物学是什么?矿物学是什么?
背景情况:
- 阿波罗11号任务返回了月球样本,包括微粒和细粒.
- 了解月球矿物质的冲击效应对于解释撞击历史至关重要.
研究的目的:
- 为了研究阿波罗11号矿物碎片中冲击诱导的微结构效应.
- 为了确定这些月球材料所经历的冲击压力.
主要方法:
- 矿物碎片 (clinopyroxene,olivine) 的微观结构分析.
- 检查冲击诱导的融特征 (球体,玻璃碎片).
主要成果:
- 在clinopyroxene中观察到多重生,在olivine中观察到不连续性.
- 识别了冲击诱导的融特征,包括结晶的等效物.
- 推导出100至200千巴之间的弱至中等冲击压力.
结论:
- 阿波罗11号微型爆破和罚款记录了微弱到中度的冲击事件.
- 微观结构和融证据支持压力估计.
- 这些发现有助于理解月球撞击过程.
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