华北克拉通胶北地体蓬莱群辅子夼组碎屑锆石U-Pb定年及其地质意义

王宏宇; 王义龙; 刘平华; 周万蓬; 张宇佳; 张传恒

doi:10.3799/dqkx.2021.061

Volume 46 Issue 9

Oct. 2021

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Article Navigation > Earth Science > 2021 > 46(9): 3074-3090

Wang Hongyu, Wang Yilong, Liu Pinghua, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Detrital Zircon U-Pb Dating of the Fuzikuang Formation, Penglai Group in Jiaobei Terrane, North China Craton and Its Geological Significance. Earth Science, 46(9): 3074-3090. doi: 10.3799/dqkx.2021.061

Citation:

Wang Hongyu, Wang Yilong, Liu Pinghua, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Detrital Zircon U-Pb Dating of the Fuzikuang Formation, Penglai Group in Jiaobei Terrane, North China Craton and Its Geological Significance. Earth Science, 46(9): 3074-3090. doi: 10.3799/dqkx.2021.061

Citation:

Wang Hongyu, Wang Yilong, Liu Pinghua, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Detrital Zircon U-Pb Dating of the Fuzikuang Formation, Penglai Group in Jiaobei Terrane, North China Craton and Its Geological Significance. Earth Science, 46(9): 3074-3090. doi: 10.3799/dqkx.2021.061

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Detrital Zircon U-Pb Dating of the Fuzikuang Formation, Penglai Group in Jiaobei Terrane, North China Craton and Its Geological Significance

doi: 10.3799/dqkx.2021.061

Wang Hongyu^{1
,
,},
Wang Yilong^{2, 3},
Liu Pinghua^{3
,
,
,},
Zhou Wanpeng²,
Zhang Yujia^{2, 3},
Zhang Chuanheng¹

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
School of Earth Sciences, East China University of Technology, Nanchang 330013, China
3.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2021-03-10
Available Online: 2021-10-14
Publish Date: 2021-10-14

Abstract

Abstract

The Penglai Group is an important late Precambrian sedimentary cover in Jiaobei area, which is of great significance to study the late Precambrian evolution in the southeastern margin of the North China Craton. In order to confirm the sedimentary age and provenance characteristics of the Penglai Group in the Jiaobei area, a fine-grained feldspar quartzite in the upper part of the Fuzikuang Formation, Penglai Group in the Qixia area is selected for analyses of the zircon CL image, U-Pb age and REE composition in this study. Results show that detrital zircons mainly belong to magmatic origin, with the peak ages of 1 100 Ma, 1 200 Ma and 1 600 Ma, and there are a few zircons with age older than 1.8 Ga. The youngest zircon age is 1 094±39 Ma, combined with the previous data, the sedimentary age of the Fuzikuang Formation in the Penglai Group should be limited to early Neoproterozoic. The provenance of the Penglai Group in different areas are the same in the middle and upper parts of the Fuzikuang Formation, but the provenance may change in the lower part of the Fuzikuang Formation. From regional perspective, the provenance characteristics of the Penglai Group are similar to those of the Neoproterozoic strata in the southern margin of the North China Craton, such as the Sangwon System in North Korea, and the Xihe Group in the Liaodong Peninsula, the Tumen Group in the Luxi area, the Huainan Group in Xuhuai area and the Luanchuan Group in western Henan, China. The main provenance areas are outside the North China Craton. Combined with paleomagnetic data and distribution of Meso-Neoproterozoic mafic dykes, we speculate that the southern margin of the North China Craton combined with the craton having Grenvillian orogen on it, maybe Laurentia-Siberia-Baltica Craton or Sao Franco-Congo Craton, which provided the provenance for the Penglai Group.
- Penglai Group,
- Fuzikuang Formation,
- detrital zircon U-Pb dating,
- provenance analysis,
- petrology

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References(104)

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Detrital Zircon U-Pb Dating of the Fuzikuang Formation, Penglai Group in Jiaobei Terrane, North China Craton and Its Geological Significance

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