肇事逃逸碰撞的特征

E. Asphaug
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引用次数: 9

摘要

类地行星是在一系列类似大小的碰撞中形成的,这些碰撞席卷了大多数次大天体。根据这个理论,它们被地球吸积形成了月球。类似地,星子也可能在一系列“初级巨型撞击”中完成了它们的吸积,这些撞击在大小和速度上都缩小了。本章考虑了复杂的双吸积物理,当星子生长到行星尺度,并考虑了该过程的低效如何影响星子的起源和陨石和初级小行星的多样性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Signatures of Hit-and-run Collisions
Terrestrial planets grew in a series of similar-sized collisions that swept up most of the next-largest bodies. Theia was accreted by the Earth to form the Moon according to the theory. Planetesimals likewise may have finished their accretion in a sequence of 'junior giant impacts', scaled down in size and velocity. This chapter considers the complicated physics of pairwise accretion, as planetesimals grow to planetary scales, and considers how the inefficiency of that process influences the origin of planetesimals and the diversity of meteorites and primary asteroids.
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