The bulk crustal porosity of the lunar highland may have been generated early in the Moon’s history by basin-forming impacts and then declined exponentially. A new porosity evolution model constrains the timing and sequence of basin formation.
References
Bottke, W. F. et al. Annu. Rev. Earth Planet. Sci. 45, 619–647 (2017).
Fassett, C. I. et al. Nat. Geosci. 6, 520–524 (2013).
Huang, Y. H. et al. Nat. Geosci. https://doi.org/10.1038/s41561-022-00969-4 (2022).
Stöffler, D. et al. Space Sci. Rev. 96, 9–54 (2001).
Wieczorek, M. A. et al. Science. 339, 671–675 (2013).
Wahl, D. et al. J. Geophys. Res. Planets 125, e2019JE006335 (2020).
Ding, C. et al. Geophys. Res. Lett. 47, 1–9 (2020).
Tera, F. et al. Earth Planet. Sci. Lett. 22, 1–21 (1974).
Miljković et al. Nat. Commun. 12, 5433 (2021).
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
Competing interests
The author declares no competing interests.
Rights and permissions
About this article
Cite this article
Xiao, Z. Moon’s crustal porosity records impact history. Nat. Geosci. 15, 512–513 (2022). https://doi.org/10.1038/s41561-022-00985-4
Published:
Issue Date:
DOI: https://doi.org/10.1038/s41561-022-00985-4
- Springer Nature Limited
This article is cited by
-
An overview and perspective of identifying lunar craters
Science China Earth Sciences (2024)