地球和月球之间的组成相似性的原始起源
Alessandra Mastrobuono-Battisti1, Hagai B Perets1, Sean N Raymond2
1Department of Physics, Technion, Israel Institute of Technology, Haifa 32000, Israel.
Nature
|April 10, 2015
概括
地球和月球具有相似的同位素组成,这挑战了巨大的撞击假说. 新的模拟显示,形成月球的撞击物通常具有与它们撞击的行星几乎相同的组成,支持巨型撞击场景.
科学领域:
- 行星科学 行星科学
- 天体物理学 天体物理学
- 地质化学 地质化学
背景情况:
- 巨大的撞击假说假设地球和火星大小的物体之间的碰撞形成了月球.
- 地球和月球之间的同位素相似性挑战了这一点,因为撞击物的组成应该不同.
- 其他太阳系天体呈现出不同的同位素组成.
研究的目的:
- 在行星积累模拟中调查月球形成冲击物的同位素组成.
- 为了使观测到的地球-月球同位素相似性与巨型撞击场景相协调.
主要方法:
- 进行行星积聚的模拟.
- 追踪生长行星和冲击因素的养区和组成.
- 分析行星和撞击器组成之间的统计相似性.
主要成果:
- 在同一个模拟中形成的行星显示出不同的组成.
- 巨大的撞击物表现出与其撞击的行星统计学上相似的组成.
- 很大一部分行星撞击器对显示几乎相同的组成.
结论:
- 地球和月球之间的同位素相似性是巨型撞击过程的自然结果.
- 巨大的撞击场景仍然是月球形成的可行解释.
- 模拟支持这样一个想法,即撞击物可能具有与原地球相似的组成.
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