Discovery of the Hailin impact crater in northeast China

A uniquely shaped impact structure, the Hailin impact crater, has been discovered in northeast China. The crater was formed on a granodiorite hillside and is an oval depression with asymmetric rim height and a maximum diameter of 1360 m. The bottom of the crater is filled by Quaternary sediments wit...

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Main Authors: Feng Yin, Ming Chen, Wenge Yang, Ho-kwang Mao
Format: Article
Language:English
Published: AIP Publishing LLC 2025-01-01
Series:Matter and Radiation at Extremes
Online Access:http://dx.doi.org/10.1063/5.0236993
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author Feng Yin
Ming Chen
Wenge Yang
Ho-kwang Mao
author_facet Feng Yin
Ming Chen
Wenge Yang
Ho-kwang Mao
author_sort Feng Yin
collection DOAJ
description A uniquely shaped impact structure, the Hailin impact crater, has been discovered in northeast China. The crater was formed on a granodiorite hillside and is an oval depression with asymmetric rim height and a maximum diameter of 1360 m. The bottom of the crater is filled by Quaternary sediments with large amounts of rock fragments underneath. The discovery of quartz planar deformation features in rock clasts on the crater floor provides diagnostic evidence for the impact origin of the structure. The shape of the crater is largely due to the impact having occurred on a ridge terrain. The impact event probably occurred in the late Cenozoic Era. The Hailin impact crater is the fourth confirmed Chinese impact crater.
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id doaj-art-4c3e7df4f19a4112b3748ca98bc5de6e
institution Kabale University
issn 2468-080X
language English
publishDate 2025-01-01
publisher AIP Publishing LLC
record_format Article
series Matter and Radiation at Extremes
spelling doaj-art-4c3e7df4f19a4112b3748ca98bc5de6e2025-02-03T16:33:24ZengAIP Publishing LLCMatter and Radiation at Extremes2468-080X2025-01-01101013001013001-510.1063/5.0236993Discovery of the Hailin impact crater in northeast ChinaFeng Yin0Ming Chen1Wenge Yang2Ho-kwang Mao3Center for High Pressure Science and Technology Advanced Research, Shanghai 201203, ChinaCenter for High Pressure Science and Technology Advanced Research, Shanghai 201203, ChinaCenter for High Pressure Science and Technology Advanced Research, Shanghai 201203, ChinaCenter for High Pressure Science and Technology Advanced Research, Shanghai 201203, ChinaA uniquely shaped impact structure, the Hailin impact crater, has been discovered in northeast China. The crater was formed on a granodiorite hillside and is an oval depression with asymmetric rim height and a maximum diameter of 1360 m. The bottom of the crater is filled by Quaternary sediments with large amounts of rock fragments underneath. The discovery of quartz planar deformation features in rock clasts on the crater floor provides diagnostic evidence for the impact origin of the structure. The shape of the crater is largely due to the impact having occurred on a ridge terrain. The impact event probably occurred in the late Cenozoic Era. The Hailin impact crater is the fourth confirmed Chinese impact crater.http://dx.doi.org/10.1063/5.0236993
spellingShingle Feng Yin
Ming Chen
Wenge Yang
Ho-kwang Mao
Discovery of the Hailin impact crater in northeast China
Matter and Radiation at Extremes
title Discovery of the Hailin impact crater in northeast China
title_full Discovery of the Hailin impact crater in northeast China
title_fullStr Discovery of the Hailin impact crater in northeast China
title_full_unstemmed Discovery of the Hailin impact crater in northeast China
title_short Discovery of the Hailin impact crater in northeast China
title_sort discovery of the hailin impact crater in northeast china
url http://dx.doi.org/10.1063/5.0236993
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AT mingchen discoveryofthehailinimpactcraterinnortheastchina
AT wengeyang discoveryofthehailinimpactcraterinnortheastchina
AT hokwangmao discoveryofthehailinimpactcraterinnortheastchina