Geochronology Definition of Jian'ancun Formation in Wutai Hutuo Group and Its Implications

Purposes The Hutuo Group belongs to the Early Proterozoic strata. As one of the most typical Paleoproterozoic strata in North China, the timing redefinition of the Hutuo Group is of great significance to the establishment of the early Precambrian stratigraphic chronology framework, the discussion of...

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Main Authors: Chao LI, Yong LEI, Wei HAN, Zhiqiang FENG, Jianrong LI, Tao YAN, Chenyan TANG, Jie CUI
Format: Article
Language:English
Published: Editorial Office of Journal of Taiyuan University of Technology 2024-03-01
Series:Taiyuan Ligong Daxue xuebao
Subjects:
Online Access:https://tyutjournal.tyut.edu.cn/englishpaper/show-2271.html
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author Chao LI
Yong LEI
Wei HAN
Zhiqiang FENG
Jianrong LI
Tao YAN
Chenyan TANG
Jie CUI
author_facet Chao LI
Yong LEI
Wei HAN
Zhiqiang FENG
Jianrong LI
Tao YAN
Chenyan TANG
Jie CUI
author_sort Chao LI
collection DOAJ
description Purposes The Hutuo Group belongs to the Early Proterozoic strata. As one of the most typical Paleoproterozoic strata in North China, the timing redefinition of the Hutuo Group is of great significance to the establishment of the early Precambrian stratigraphic chronology framework, the discussion of the early Precambrian geological evolution process in North China and the study of plate assembly. Methods This article conducts a detailed study of the Dongye Subgroup strata of the Hutuo Group, collecting 24 detrital zircon samples from the Jian'ancun Formation of the Hutuo Group. From 23 similar age detrital zircons, we define the weighted average age of the bottom boundary of the Hutuo Group is 2 469 Ma, and regional tectonic movements occurred in the Wutai area around 1 855 Ma. According to the 1 109 zircon ages in Hutuo Group from previous studies, we considered that the ages of >2.5 Ga are from underlying Gaofan subgroup and the maximum depositional age of Hutuo Group was early Paleoproterozoic. Findings The results show that the crust of the Wutai area was unstable at 2 376, 2 170, 2 066, 1 988, and 1 825 Ma, resulting in multiple magmatic events. The 1 825 Ma zircon age can further indicate the occurrence of the Lyuliang movement, and provide a basis for the early Proterozoic North China Craton integration.
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spelling doaj.art-64444f4942b942ab81dc673030d7211d2024-04-15T09:17:32ZengEditorial Office of Journal of Taiyuan University of TechnologyTaiyuan Ligong Daxue xuebao1007-94322024-03-0155229630510.16355/j.tyut.1007-9432.202305071007-9432(2024)02-0296-10Geochronology Definition of Jian'ancun Formation in Wutai Hutuo Group and Its ImplicationsChao LI0Yong LEI1Wei HAN2Zhiqiang FENG3Jianrong LI4Tao YAN5Chenyan TANG6Jie CUI7Shanxi Geological Museum, Taiyuan 030021, ChinaCollege of Resources and Environment, Shanxi Agricultural University, Taigu 030801, ChinaDepartment of Earth Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, ChinaDepartment of Earth Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, ChinaShanxi Institute of Geological Survey Co., LTD, Taiyuan 030006, ChinaShanxi Institute of Geological Survey Co., LTD, Taiyuan 030006, ChinaShanxi Land-Care Planning and Design Consulting Co., Ltd, Taiyuan 030024, ChinaTai Yuan Foreign Language School, Taiyuan 030024, ChinaPurposes The Hutuo Group belongs to the Early Proterozoic strata. As one of the most typical Paleoproterozoic strata in North China, the timing redefinition of the Hutuo Group is of great significance to the establishment of the early Precambrian stratigraphic chronology framework, the discussion of the early Precambrian geological evolution process in North China and the study of plate assembly. Methods This article conducts a detailed study of the Dongye Subgroup strata of the Hutuo Group, collecting 24 detrital zircon samples from the Jian'ancun Formation of the Hutuo Group. From 23 similar age detrital zircons, we define the weighted average age of the bottom boundary of the Hutuo Group is 2 469 Ma, and regional tectonic movements occurred in the Wutai area around 1 855 Ma. According to the 1 109 zircon ages in Hutuo Group from previous studies, we considered that the ages of >2.5 Ga are from underlying Gaofan subgroup and the maximum depositional age of Hutuo Group was early Paleoproterozoic. Findings The results show that the crust of the Wutai area was unstable at 2 376, 2 170, 2 066, 1 988, and 1 825 Ma, resulting in multiple magmatic events. The 1 825 Ma zircon age can further indicate the occurrence of the Lyuliang movement, and provide a basis for the early Proterozoic North China Craton integration.https://tyutjournal.tyut.edu.cn/englishpaper/show-2271.htmlwutai mountainjian'ancun formationzircon u-pb datinghutuo groupearly paleoproterozoic
spellingShingle Chao LI
Yong LEI
Wei HAN
Zhiqiang FENG
Jianrong LI
Tao YAN
Chenyan TANG
Jie CUI
Geochronology Definition of Jian'ancun Formation in Wutai Hutuo Group and Its Implications
Taiyuan Ligong Daxue xuebao
wutai mountain
jian'ancun formation
zircon u-pb dating
hutuo group
early paleoproterozoic
title Geochronology Definition of Jian'ancun Formation in Wutai Hutuo Group and Its Implications
title_full Geochronology Definition of Jian'ancun Formation in Wutai Hutuo Group and Its Implications
title_fullStr Geochronology Definition of Jian'ancun Formation in Wutai Hutuo Group and Its Implications
title_full_unstemmed Geochronology Definition of Jian'ancun Formation in Wutai Hutuo Group and Its Implications
title_short Geochronology Definition of Jian'ancun Formation in Wutai Hutuo Group and Its Implications
title_sort geochronology definition of jian ancun formation in wutai hutuo group and its implications
topic wutai mountain
jian'ancun formation
zircon u-pb dating
hutuo group
early paleoproterozoic
url https://tyutjournal.tyut.edu.cn/englishpaper/show-2271.html
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