Lunar Evolution Analysis Based on Numerical Simulations of Typical Lunar Impact Craters

Impact craters are one of the most important landforms on the lunar surface, playing a crucial role in the formation and later evolution of the Moon. For example, as a primary source of remote sensing observations and lunar samples, lunar regolith is predominantly composed of impact ejecta. Based on...

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Main Authors: Zongyu Yue, Huacheng Li, Nan Zhang, Sheng Gou, Yangting Lin
Format: Article
Language:English
Published: American Association for the Advancement of Science (AAAS) 2023-01-01
Series:Space: Science & Technology
Online Access:https://spj.science.org/doi/10.34133/space.0084
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author Zongyu Yue
Huacheng Li
Nan Zhang
Sheng Gou
Yangting Lin
author_facet Zongyu Yue
Huacheng Li
Nan Zhang
Sheng Gou
Yangting Lin
author_sort Zongyu Yue
collection DOAJ
description Impact craters are one of the most important landforms on the lunar surface, playing a crucial role in the formation and later evolution of the Moon. For example, as a primary source of remote sensing observations and lunar samples, lunar regolith is predominantly composed of impact ejecta. Based on their morphologies, lunar impact craters with increasing sizes can be classified into simple craters, complex craters, and multiring basins, and they play different roles in lunar evolution. In our study, we conducted numerical simulations of the South Pole-Aitken basin and the Orientale basin on the lunar surface, as well as the Aristarchus complex crater and the Zhinyu simple crater. The resultant effects of them are further analyzed. Because Zhinyu crater is relatively close to the Chang’e-4 landing site, while Aristarchus crater is relatively close to the Chang’e-5 landing site, their simulation results have direct significance for interpreting the corresponding exploration data from both missions. The numerical simulation results demonstrate that the formation of large basins not only affects the subsurface structure within the basin but also significantly disturbs the surrounding geological layers. Complex and simple craters mainly disturb the subsurface layers within the crater, but complex craters can cause uplift of the underlying strata. These impact processes dominate the primary geological framework of the lunar surface, depositing ejecta materials of varying thicknesses from different depths, which has important implications for future sample collection missions. In conclusion, impact processes are one of the primary driving forces in the lunar evolution.
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spelling doaj.art-7eb7d18416574cfd81b09ef2802784f72023-12-06T17:34:33ZengAmerican Association for the Advancement of Science (AAAS)Space: Science & Technology2692-76592023-01-01310.34133/space.0084Lunar Evolution Analysis Based on Numerical Simulations of Typical Lunar Impact CratersZongyu Yue0Huacheng Li1Nan Zhang2Sheng Gou3Yangting Lin4Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.School of Earth and Space Sciences, Peking University, Beijing 100871, China.Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.Impact craters are one of the most important landforms on the lunar surface, playing a crucial role in the formation and later evolution of the Moon. For example, as a primary source of remote sensing observations and lunar samples, lunar regolith is predominantly composed of impact ejecta. Based on their morphologies, lunar impact craters with increasing sizes can be classified into simple craters, complex craters, and multiring basins, and they play different roles in lunar evolution. In our study, we conducted numerical simulations of the South Pole-Aitken basin and the Orientale basin on the lunar surface, as well as the Aristarchus complex crater and the Zhinyu simple crater. The resultant effects of them are further analyzed. Because Zhinyu crater is relatively close to the Chang’e-4 landing site, while Aristarchus crater is relatively close to the Chang’e-5 landing site, their simulation results have direct significance for interpreting the corresponding exploration data from both missions. The numerical simulation results demonstrate that the formation of large basins not only affects the subsurface structure within the basin but also significantly disturbs the surrounding geological layers. Complex and simple craters mainly disturb the subsurface layers within the crater, but complex craters can cause uplift of the underlying strata. These impact processes dominate the primary geological framework of the lunar surface, depositing ejecta materials of varying thicknesses from different depths, which has important implications for future sample collection missions. In conclusion, impact processes are one of the primary driving forces in the lunar evolution.https://spj.science.org/doi/10.34133/space.0084
spellingShingle Zongyu Yue
Huacheng Li
Nan Zhang
Sheng Gou
Yangting Lin
Lunar Evolution Analysis Based on Numerical Simulations of Typical Lunar Impact Craters
Space: Science & Technology
title Lunar Evolution Analysis Based on Numerical Simulations of Typical Lunar Impact Craters
title_full Lunar Evolution Analysis Based on Numerical Simulations of Typical Lunar Impact Craters
title_fullStr Lunar Evolution Analysis Based on Numerical Simulations of Typical Lunar Impact Craters
title_full_unstemmed Lunar Evolution Analysis Based on Numerical Simulations of Typical Lunar Impact Craters
title_short Lunar Evolution Analysis Based on Numerical Simulations of Typical Lunar Impact Craters
title_sort lunar evolution analysis based on numerical simulations of typical lunar impact craters
url https://spj.science.org/doi/10.34133/space.0084
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AT huachengli lunarevolutionanalysisbasedonnumericalsimulationsoftypicallunarimpactcraters
AT nanzhang lunarevolutionanalysisbasedonnumericalsimulationsoftypicallunarimpactcraters
AT shenggou lunarevolutionanalysisbasedonnumericalsimulationsoftypicallunarimpactcraters
AT yangtinglin lunarevolutionanalysisbasedonnumericalsimulationsoftypicallunarimpactcraters