論文

査読有り 最終著者
2022年5月

Resurfacing processes constrained by crater distribution on Ryugu

Icarus
  • Naofumi Takaki
  • Yuichiro Cho
  • Tomokatsu Morota
  • Eri Tatsumi
  • Rie Honda
  • Shingo Kameda
  • Yasuhiro Yokota
  • Naoya Sakatani
  • Toru Kouyama
  • Masahiko Hayakawa
  • Moe Matsuoka
  • Manabu Yamada
  • Chikatoshi Honda
  • Hidehiko Suzuki
  • Kazuo Yoshioka
  • Kazunori Ogawa
  • Hirotaka Sawada
  • Patrick Michel
  • Seiji Sugita
  • 全て表示

377
開始ページ
114911
終了ページ
114911
記述言語
英語
掲載種別
研究論文(学術雑誌)
DOI
10.1016/j.icarus.2022.114911
出版者・発行元
Elsevier BV

Understanding the geological modification processes on asteroids is fundamental for elucidating their surface evolution. Images of small asteroids from spacecrafts show a depletion in smaller craters. Seismic shaking was considered to be responsible for erasing such small craters and the main driver modifying the geology of asteroids. However, a recent artificial impact experiment on asteroid Ryugu conducted by the Japanese Hayabusa2 spacecraft revealed minimal seismic efficiency on the asteroid. To investigate whether a standard seismic shaking model can reproduce the observed crater record, we analyzed the crater distributions on four asteroids, i.e., Eros, Itokawa, Ryugu, and Bennu, using crater production functions under cohesionless conditions. Crater retention ages were estimated as a function of crater diameter for the four asteroids using the crater size-frequency distribution and crater production function estimated for each asteroid. We obtained the relation between a crater retention age t and crater diameter D in the form of power-law function (t ∝ Da).We found that the power-law indices a are inconsistent with diffusion processes (e.g., seismic shaking, where a = 2). This result suggests that seismic shaking models based on a linear diffusion equation cannot explain the crater distribution on the small asteroids. Alternative crater obliteration processes include surface flows suggested by geomorphological and spectral features of Ryugu. Using the crater statistics, we also show that the vertical mixing of the Ryugu material at the depths shallower than 1 m occurs in 103–105 yr by cratering. This rapid resurfacing and replacement of the surface layer in the short timescale would account for the decrease in space weathering rate suggested by previous studies. Furthermore, the timescale required for vertically transporting Ryugu materials to the depths of 2–4 m (104–106 yr), where cosmic rays would not reach, can be compared with the cosmic-ray exposure ages of returned samples. This comparison can be used to constrain the distribution of impactors that collide with Ryugu.

リンク情報
DOI
https://doi.org/10.1016/j.icarus.2022.114911
Scopus
https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85124203778&origin=inward
Scopus Citedby
https://www.scopus.com/inward/citedby.uri?partnerID=HzOxMe3b&scp=85124203778&origin=inward
ID情報
  • DOI : 10.1016/j.icarus.2022.114911
  • ISSN : 0019-1035
  • eISSN : 1090-2643
  • SCOPUS ID : 85124203778

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