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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Published in:Geophysical Research Letters
Main Authors: Huaqing Cao, Yi Xu, Luyuan Xu, Ling Zhang, Roberto Bugiolacchi, Feng Zhang
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2022GL101413
https://doaj.org/article/f515b92de7bb4cd28cf8f4cb9f551976
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spelling 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
op_collection_id 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
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