Lunar regolith and substructure at Chang’E-4 landing site in South Pole–Aitken basin
Author:
Publisher
Springer Science and Business Media LLC
Subject
Astronomy and Astrophysics
Link
https://www.nature.com/articles/s41550-020-1197-x.pdf
Reference62 articles.
1. Ohtake, M. et al. Geologic structure generated by large-impact basin formation observed at the South Pole–Aitken basin on the Moon. Geophys. Res. Lett. 41, 2738–2745 (2014).
2. Melosh, H. J. et al. South Pole–Aitken basin ejecta reveal the Moon’s upper mantle. Geology 45, 1063–1066 (2017).
3. Moriarty, D. P. III & Pieters, C. M. The character of South Pole–Aitken basin: patterns of surface and subsurface composition. J. Geophys. Res. Planets 123, 729–747 (2018).
4. Li, C. et al. Chang’e-4 initial spectroscopic identification of lunar far-side mantle-derived material. Nature 569, 378–382 (2019).
5. Wu, W. et al. Lunar farside to be explored by Chang’e-4. Nat. Geosci. 12, 222–223 (2019).
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