埃及的卡米尔火山口在埃及
Luigi Folco1, Mario Di Martino, Ahmed El Barkooky
1Museo Nazionale dell'Antartide Università di Siena, Via Laterina 8, 53100 Siena, Italy. folco@unisi.it
概括
在埃及,一个原始的45米撞击坑揭示了铁石可以完好无损地在进入大气层时幸存下来. 这一发现挑战了当前对地球超高速撞击的模型.
科学领域:
- 地质地质地质地质地质地
- 行星科学 行星科学
- 冲击石坑的形成
背景情况:
- 纯净的光线结构在地球上很少见,通常在没有大气层的天体上发现.
- 了解超高速影响对于行星科学和地球危险评估至关重要.
研究的目的:
- 报告在埃及南部发现了一个独特的,原始的撞击坑.
- 调查撞击物质的性质和由此产生的冲击变形.
- 挑战现有的地质物理模型关于铁石进入大气层.
主要方法:
- 地质实地调查以确定和描述冲击结构.
- 对石碎片进行分析,以确定其组成和来源.
- 对岩石样本进行显微镜检查,以确定冲击变态特征.
主要成果:
- 发现了一个直径45米的撞击坑,其光线结构保存良好.
- 石坑与铁石撞击器的关联.
- 在石坑岩石中,有显著的冲击变形的证据.
- 地面数据与预测大铁石在进入大气中的大量碎片化模型相矛盾.
结论:
- 埃及的火山口提供了一个罕见的陆地原始撞击结构的例子.
- 几十重的铁石可以以最小的碎片化穿透地球大气层,这与目前的模型相反.
- 这一发现为小规模超高速对地球行星地的影响提供了新的见解.
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