From Schrödinger to Von Kármán: An Intriguing New Geological Structure Revealed by the Chang'e‐4 Lunar Penetrating Radar
Abstract Since early 2019, the Lunar Penetrating Radar (LPR) onboard Chang'e‐4 (CE‐4)’s Yutu‐2 rover has been gathering data relating to the subsurface structure of the Von Kármán crater within the South Pole‐Aitken Basin (SPA) on the lunar farside. Low‐frequency radar data have the potential o...
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ftdoajarticles:oai:doaj.org/article:f515b92de7bb4cd28cf8f4cb9f551976 2024-09-15T18:36:46+00:00 From Schrödinger to Von Kármán: An Intriguing New Geological Structure Revealed by the Chang'e‐4 Lunar Penetrating Radar Huaqing Cao Yi Xu Luyuan Xu Ling Zhang Roberto Bugiolacchi Feng Zhang 2023-01-01T00:00:00Z https://doi.org/10.1029/2022GL101413 https://doaj.org/article/f515b92de7bb4cd28cf8f4cb9f551976 EN eng Wiley https://doi.org/10.1029/2022GL101413 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL101413 https://doaj.org/article/f515b92de7bb4cd28cf8f4cb9f551976 Geophysical Research Letters, Vol 50, Iss 2, Pp n/a-n/a (2023) the Moon ground penetrating radar Chang'e‐4 mission impact ejecta Schrödinger basin Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2022GL101413 2024-08-05T17:49:23Z Abstract Since early 2019, the Lunar Penetrating Radar (LPR) onboard Chang'e‐4 (CE‐4)’s Yutu‐2 rover has been gathering data relating to the subsurface structure of the Von Kármán crater within the South Pole‐Aitken Basin (SPA) on the lunar farside. Low‐frequency radar data have the potential of carrying geological information of about 300 m worth of strata below the traversed path. Forty‐two days’ data have revealed a bifurcated structure within the layered structure beneath the CE‐4 surveying area for the first time, affecting the overlying reflectors between 90 and 310 m. This study suggests that, based on the morphological characteristics, thickness, depth (timing sequence) and direction of the newly found structure, its origin might be linked to the deposition of ejecta from the Schrödinger impact. The local stratigraphy is interpreted as consisting of distinct geological layers, corresponding to the superposition of ejecta from different impact craters, paleo‐regolith, and basaltic lava flows. Article in Journal/Newspaper South pole Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 2 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
the Moon ground penetrating radar Chang'e‐4 mission impact ejecta Schrödinger basin Geophysics. Cosmic physics QC801-809 |
spellingShingle |
the Moon ground penetrating radar Chang'e‐4 mission impact ejecta Schrödinger basin Geophysics. Cosmic physics QC801-809 Huaqing Cao Yi Xu Luyuan Xu Ling Zhang Roberto Bugiolacchi Feng Zhang From Schrödinger to Von Kármán: An Intriguing New Geological Structure Revealed by the Chang'e‐4 Lunar Penetrating Radar |
topic_facet |
the Moon ground penetrating radar Chang'e‐4 mission impact ejecta Schrödinger basin Geophysics. Cosmic physics QC801-809 |
description |
Abstract Since early 2019, the Lunar Penetrating Radar (LPR) onboard Chang'e‐4 (CE‐4)’s Yutu‐2 rover has been gathering data relating to the subsurface structure of the Von Kármán crater within the South Pole‐Aitken Basin (SPA) on the lunar farside. Low‐frequency radar data have the potential of carrying geological information of about 300 m worth of strata below the traversed path. Forty‐two days’ data have revealed a bifurcated structure within the layered structure beneath the CE‐4 surveying area for the first time, affecting the overlying reflectors between 90 and 310 m. This study suggests that, based on the morphological characteristics, thickness, depth (timing sequence) and direction of the newly found structure, its origin might be linked to the deposition of ejecta from the Schrödinger impact. The local stratigraphy is interpreted as consisting of distinct geological layers, corresponding to the superposition of ejecta from different impact craters, paleo‐regolith, and basaltic lava flows. |
format |
Article in Journal/Newspaper |
author |
Huaqing Cao Yi Xu Luyuan Xu Ling Zhang Roberto Bugiolacchi Feng Zhang |
author_facet |
Huaqing Cao Yi Xu Luyuan Xu Ling Zhang Roberto Bugiolacchi Feng Zhang |
author_sort |
Huaqing Cao |
title |
From Schrödinger to Von Kármán: An Intriguing New Geological Structure Revealed by the Chang'e‐4 Lunar Penetrating Radar |
title_short |
From Schrödinger to Von Kármán: An Intriguing New Geological Structure Revealed by the Chang'e‐4 Lunar Penetrating Radar |
title_full |
From Schrödinger to Von Kármán: An Intriguing New Geological Structure Revealed by the Chang'e‐4 Lunar Penetrating Radar |
title_fullStr |
From Schrödinger to Von Kármán: An Intriguing New Geological Structure Revealed by the Chang'e‐4 Lunar Penetrating Radar |
title_full_unstemmed |
From Schrödinger to Von Kármán: An Intriguing New Geological Structure Revealed by the Chang'e‐4 Lunar Penetrating Radar |
title_sort |
from schrödinger to von kármán: an intriguing new geological structure revealed by the chang'e‐4 lunar penetrating radar |
publisher |
Wiley |
publishDate |
2023 |
url |
https://doi.org/10.1029/2022GL101413 https://doaj.org/article/f515b92de7bb4cd28cf8f4cb9f551976 |
genre |
South pole |
genre_facet |
South pole |
op_source |
Geophysical Research Letters, Vol 50, Iss 2, Pp n/a-n/a (2023) |
op_relation |
https://doi.org/10.1029/2022GL101413 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL101413 https://doaj.org/article/f515b92de7bb4cd28cf8f4cb9f551976 |
op_doi |
https://doi.org/10.1029/2022GL101413 |
container_title |
Geophysical Research Letters |
container_volume |
50 |
container_issue |
2 |
_version_ |
1810480487264681984 |